فهرست مطالب behrouz sobhani

Land surface temperature (LST) is a key physical parameter of land surface processes, at local and global scales, which is a combination of all results from the land surface and the energy flow between the surface and the atmosphere. Earth surface temperature is an important indicator related to climatic, meteorological, hydrological and environmental phenomena and processes. Currently, data from meteorological stations are the most important decision-making reference in this case (Baidy et al., 2013: 517). What is considered as a basic defect in monitoring the temperature of the earth's surface is the lack of sufficient meteorological stations to know the temperature values in places without stations. Considering the limited information, the need to use remote sensing technology with time conditions, along with the feature of continuity and data collection in wide ranges, can be very efficient (Kake Memi et al., 2019).Soil moisture is the amount of water stored in soil particles and is affected by factors such as precipitation, temperature and other soil properties (Pandi et al., 2020: 1). Estimating soil moisture is of great value for weather forecasting, climate change monitoring, and flood monitoring (Beau et al., 2018). Remote sensing techniques provide tools for mapping soil moisture at large spatial and temporal scales. Remote sensing can be effectively used to estimate soil moisture because soil light reflectance and thermal emission are highly correlated with soil moisture (Acharya et al., 2022: 2).Meteorological and hydrogeological studies of the Sentinel satellite series have been developed by the European Space Agency (ESA) to support the services of the European mission and the demands of the Copernicus program (Zarei et al., 2021: 3980); The first three Sentinel missions contribute to the understanding of the Earth system by detecting, monitoring, and evaluating changes in the ocean, troposphere, and land components (Ruskas et al., 2016: 1).

The studied area is Nair city. This city covers 8% of the total area of Ardabil province with an area of 1495 square kilometers. It is located at 47 degrees 59 minutes east longitude and 38 degrees 2 minutes north latitude. This city of Nir is located 35 kilometers west of Ardabil between Sablan and Bezgosh mountains. In this study, Sentinel 2 satellite images have been prepared for the date of 12/7/2022, and then atmospheric and radiometric corrections were made in ENVI 5.6 software, and a part of the images was cut based on the study area. After the atmospheric and radiometric correction of the image, the land use classification map was prepared in eCognition 9 software using the nearest neighbor method of the object-oriented algorithm; There are two main steps in image base object classification. The first step is image segmentation, which divides the image into separate areas or objects (segments) based on a similar spectral and spatial pattern. After segmentation, the second step is to relate the image segments using spectral and shape statistics, texture parameters and topological information. To perform this method, the results of different scales were analyzed. Finally, considering the scale of 60 and the amount of softness and compression, respectively, 4 0.0 and 0.6 segmentation was done. After segmentation of the study area, they were classified into seven classes: irrigated agriculture, rainfed agriculture, residential area, water areas, snow cover, pasture and communication road; Then, the kappa coefficient and accuracy were estimated for validation. Sentinel 2 image was also used to calculate soil moisture using OPTRAM method. To perform this method, first NDVI and STR index were calculated and then soil moisture value was determined using these two indices.In the continuation of the research, to calculate the temperature of the earth's surface, the daily temperature product of Sentinel 3 images related to the time of 7/11/2022 was prepared for the studied area; And in the SNAP software, the temperature of the earth's surface was estimated. The Sentinel 3 temperature product is an official level 2 product and has a spatial resolution of 1 km. It provides estimates of LST and some related parameters, e.g. LST uncertainty, normalized difference vegetation index (NDVI), vegetation type (biome), atmospheric column water vapor content (CWVC) and parameters related to LST retrieval. has After extracting maps of surface temperature and soil moisture using satellite images, the correlation between the dependent variable of humidity and the independent variable of temperature has been investigated using geographic weighted regression. calculating In this research, in the first step, the classification of land use in seven classes of irrigated agriculture, rainfed agriculture, pasture, residential area, water areas, snow cover and communication road has been done using the object-oriented method in eCognition software. The accuracy of this classification has an overall accuracy of 99% and a kappa coefficient of 98%, which has achieved acceptable results due to the use of Sentinel 2 images. One of the influencing factors on land suitability for different uses is soil surface temperature. In this study, the temperature products of Sentinel 3 images were used to check the soil surface temperature. One of the factors affected by climate and temperature is soil moisture; In this way, Sentinel 2 images and OPTRAM method have been used to estimate soil moisture. Examining the results shows that the temperature of the ground surface and the amount of soil moisture are completely dependent on the nature of the types of use. The highest average temperature related to pasture use is 43 degrees Celsius and the lowest average temperature related to snow and water use is 34 and 37 degrees, respectively. Examining the soil moisture of each land use shows that water areas have the highest average humidity and residential areas have the lowest average. Based on the results, there is a direct and inverse relationship between soil surface moisture, vegetation density and surface temperature. The presence of moisture on the surface of the soil and vegetation leads to a decrease in the temperature of the earth's surface. So that dry lands, or in other words, low humidity, as well as lands with low density vegetation, correspond to the areas that show high temperature in thermal images.

Awareness of the environment and better understanding of the climate of each region is very necessary for the future to analyze the current situation of beekeeping in order to advance the goals in this field. In addition to weather factors and climatic variables, the temperature factor plays an essential role in creating a balance between honeybees and the environment. It should be noted that one of the most common problems in the growth of honeybees is unusual changes in environmental conditions, such as a sudden increase or decrease in temperature in mountainous areas, which increases the importance of studying this matter. In this research, due to the high importance of temperature, 20 years of daily temperature statistics of meteorological stations have been used. The dates of occurrence of the first and last temperatures of zero degrees were investigated and used to identify the time of inactive temperatures, to calculate the deviation from the optimal temperature (22 degrees) in the minimum winter consumption of this beneficial insect. The results of station estimates were also zoned using GIS software. The results showed that according to the calendar obtained from the cold months of the year, the thermal conditions in the last four months of the year, based on the occurrence of low temperatures from December to March, are unsuitable for biological activities in the high areas of Sablan, and the colonies should migrate to an altitude of 1000 meters and be monitored. The most optimal months of the year for the activity of bees in the highlands with the results obtained start from May because a huge source of flowering plants grow in these areas. By adapting the temperature thresholds of honeybees to the weather conditions of each region, it is possible to help move the colonies at the right times for the development of beekeeping, and also prevent the significant reduction of the colony population due to the death of bees in cold areas and bring it to the lowest possible level. Migrated to be monitored. The most optimal months of the year for the activity of bees in the highlands with the results obtained start from May because a huge source of flowering plants grow in these areas. By matching the temperature thresholds of honey bees with the weather conditions of each region, it is possible to help move the colonies at the right times for the development of beekeeping and also prevent the significant reduction of the colony population due to the death of bees in cold areas and reduce it to the minimum. as much as possible. Beekeeping has long been one of the important branches of agriculture due to its pollination and valuable products (Allen et al., 1998). The honey bee performs more than 90% of commercial pollination services because it is considered one of the most important pollinators worldwide (Morse and Calderon, 2000). It should be pointed out that Iran's honey bee colonies are a type of common honey bee that are highly dependent on weather conditions . Coordination of beekeeping activities with climatic factors and its temporal and spatial patterns is one of the important issues regarding growth and breeding . Colony health, production efficiency and productivity in beekeeping are all affected by environmental conditions, especially climate. (Haig, 2006). By matching the vital thresholds of this creature with the climatic conditions of different places, it is possible to take advantage of the maximum climatic potential of the regions in the field of bee breeding. The most important aspect of keeping and rearing honey bees is coordinating beekeeping activities with geographical and climatic conditions and its temporal and spatial changes . With the occurrence of frost, many animal activities are affected, and the honey bee, which is a cold-blooded insect, is affected by the surrounding temperature and reacts to this temperature. It should be kept in mind that the development of beekeeping has a close relationship with weather conditions and the time of moving colonies depends on this factor . In the annual climatic calendar of the growth of honey bee colonies, two active and inactive periods have been identified, and in the cold months of the year, the inactive periods start and special care is taken, however, there is a sharp decrease in the population and death of the colony. We are at the end of winter, which is one of the inhibiting factors for using bee pollination services and other products. The loss of the queen due to changes in environmental conditions such as: Temperature, high humidity and prolonged cold in mountainous areas and lack of food in hives are among the most common problems of bee breeding in very low temperatures).Winter deaths and reduction of bee colony population in cold regions, an important part of which is due to environmental and climatic conditions, increase the importance of studying this matter (Pettis et al., 2010). With the climate calendar in hand and the proper location of the apiaries in the cold months of the year by the beekeepers, we will see a significant reduction in losses, business improvement and more productivity. A lot of research has been done in the field of honey bee wintering all over the world, which shows the close relationship between the cold winter weather and the temperature of the investigated environment, and the result shows that the minimum consumption of honey in large colonies is in the temperature range of -10 and 10+ degrees Celsius in temperate regions. ). Researches show that in relation to minimum winter honey consumption of bee colonies, the temperature reaches 4 to 5 degrees Celsius. By examining the effects of climate changes on the population of colonies and their diseases, it was found that considering the climatic conditions plays an essential role in beekeeping management .The research conducted in relation to the effect of climate change on a micro scale and its impact on the migration conditions of colonies in high altitudes were investigated and an advanced monitoring system was proposed ). The effects of different times of the day, temperature, humidity and air pressure on the flight of various types of stingless bees were studied and the results showed that the flight activities of these types of bees are affected by atmospheric conditions and the elements of day length, heat, humidity and pressure.

Awareness of the environment and better understanding of the climate of each region is very necessary for the future to analyze the current situation of beekeeping in order to advance the goals in this field. In addition to weather factors and climatic variables, the temperature factor plays an essential role in creating a balance between honeybees and the environment. It should be noted that one of the most common problems in the growth of honeybees is unusual changes in environmental conditions, such as a sudden increase or decrease in temperature in mountainous areas, which increases the importance of studying this matter. In this research, due to the high importance of temperature, 20 years of daily temperature statistics of meteorological stations have been used. The dates of occurrence of the first and last temperatures of zero degrees were investigated and used to identify the time of inactive temperatures, to calculate the deviation from the optimal temperature (22 degrees) in the minimum winter consumption of this beneficial insect. The results of station estimates were also zoned using GIS software. The results showed that according to the calendar obtained from the cold months of the year, the thermal conditions in the last four months of the year, based on the occurrence of low temperatures from December to March, are unsuitable for biological activities in the high areas of Sablan, and the colonies should migrate to an altitude of 1000 meters and be monitored. The most optimal months of the year for the activity of bees in the highlands with the results obtained start from May because a huge source of flowering plants grow in these areas. By adapting the temperature thresholds of honeybees to the weather conditions of each region, it is possible to help move the colonies at the right times for the development of beekeeping, and also prevent the significant reduction of the colony population due to the death of bees in cold areas and bring it to the lowest possible level. Migrated to be monitored. The most optimal months of the year for the activity of bees in the highlands with the results obtained start from May because a huge source of flowering plants grow in these areas. By matching the temperature thresholds of honey bees with the weather conditions of each region, it is possible to help move the colonies at the right times for the development of beekeeping and also prevent the significant reduction of the colony population due to the death of bees in cold areas and reduce it to the minimum. as much as possible. Beekeeping has long been one of the important branches of agriculture due to its pollination and valuable products (Allen et al., 1998). The honey bee performs more than 90% of commercial pollination services because it is considered one of the most important pollinators worldwide (Morse and Calderon, 2000). It should be pointed out that Iran's honey bee colonies are a type of common honey bee that are highly dependent on weather conditions . Coordination of beekeeping activities with climatic factors and its temporal and spatial patterns is one of the important issues regarding growth and breeding . Colony health, production efficiency and productivity in beekeeping are all affected by environmental conditions, especially climate. (Haig, 2006). By matching the vital thresholds of this creature with the climatic conditions of different places, it is possible to take advantage of the maximum climatic potential of the regions in the field of bee breeding. The most important aspect of keeping and rearing honey bees is coordinating beekeeping activities with geographical and climatic conditions and its temporal and spatial changes . With the occurrence of frost, many animal activities are affected, and the honey bee, which is a cold-blooded insect, is affected by the surrounding temperature and reacts to this temperature. It should be kept in mind that the development of beekeeping has a close relationship with weather conditions and the time of moving colonies depends on this factor . In the annual climatic calendar of the growth of honey bee colonies, two active and inactive periods have been identified, and in the cold months of the year, the inactive periods start and special care is taken, however, there is a sharp decrease in the population and death of the colony. We are at the end of winter, which is one of the inhibiting factors for using bee pollination services and other products. The loss of the queen due to changes in environmental conditions such as: Temperature, high humidity and prolonged cold in mountainous areas and lack of food in hives are among the most common problems of bee breeding in very low temperatures).Winter deaths and reduction of bee colony population in cold regions, an important part of which is due to environmental and climatic conditions, increase the importance of studying this matter (Pettis et al., 2010). With the climate calendar in hand and the proper location of the apiaries in the cold months of the year by the beekeepers, we will see a significant reduction in losses, business improvement and more productivity. A lot of research has been done in the field of honey bee wintering all over the world, which shows the close relationship between the cold winter weather and the temperature of the investigated environment, and the result shows that the minimum consumption of honey in large colonies is in the temperature range of -10 and 10+ degrees Celsius in temperate regions. ). Researches show that in relation to minimum winter honey consumption of bee colonies, the temperature reaches 4 to 5 degrees Celsius. By examining the effects of climate changes on the population of colonies and their diseases, it was found that considering the climatic conditions plays an essential role in beekeeping management .The research conducted in relation to the effect of climate change on a micro scale and its impact on the migration conditions of colonies in high altitudes were investigated and an advanced monitoring system was proposed ). The effects of different times of the day, temperature, humidity and air pressure on the flight of various types of stingless bees were studied and the results showed that the flight activities of these types of bees are affected by atmospheric conditions and the elements of day length, heat, humidity and pressure.

Awareness of the environment and better understanding of the climate of each region is very necessary for the future to analyze the current situation of beekeeping in order to advance the goals in this field. In addition to weather factors and climatic variables, the temperature factor plays an essential role in creating a balance between honeybees and the environment. It should be noted that one of the most common problems in the growth of honeybees is unusual changes in environmental conditions, such as a sudden increase or decrease in temperature in mountainous areas, which increases the importance of studying this matter. In this research, due to the high importance of temperature, 20 years of daily temperature statistics of meteorological stations have been used. The dates of occurrence of the first and last temperatures of zero degrees were investigated and used to identify the time of inactive temperatures, to calculate the deviation from the optimal temperature (22 degrees) in the minimum winter consumption of this beneficial insect. The results of station estimates were also zoned using GIS software. The results showed that according to the calendar obtained from the cold months of the year, the thermal conditions in the last four months of the year, based on the occurrence of low temperatures from December to March, are unsuitable for biological activities in the high areas of Sablan, and the colonies should migrate to an altitude of 1000 meters and be monitored. The most optimal months of the year for the activity of bees in the highlands with the results obtained start from May because a huge source of flowering plants grow in these areas. By adapting the temperature thresholds of honeybees to the weather conditions of each region, it is possible to help move the colonies at the right times for the development of beekeeping, and also prevent the significant reduction of the colony population due to the death of bees in cold areas and bring it to the lowest possible level. Migrated to be monitored. The most optimal months of the year for the activity of bees in the highlands with the results obtained start from May because a huge source of flowering plants grow in these areas. By matching the temperature thresholds of honey bees with the weather conditions of each region, it is possible to help move the colonies at the right times for the development of beekeeping and also prevent the significant reduction of the colony population due to the death of bees in cold areas and reduce it to the minimum. as much as possible. Beekeeping has long been one of the important branches of agriculture due to its pollination and valuable products (Allen et al., 1998). The honey bee performs more than 90% of commercial pollination services because it is considered one of the most important pollinators worldwide (Morse and Calderon, 2000). It should be pointed out that Iran's honey bee colonies are a type of common honey bee that are highly dependent on weather conditions . Coordination of beekeeping activities with climatic factors and its temporal and spatial patterns is one of the important issues regarding growth and breeding . Colony health, production efficiency and productivity in beekeeping are all affected by environmental conditions, especially climate. (Haig, 2006). By matching the vital thresholds of this creature with the climatic conditions of different places, it is possible to take advantage of the maximum climatic potential of the regions in the field of bee breeding. The most important aspect of keeping and rearing honey bees is coordinating beekeeping activities with geographical and climatic conditions and its temporal and spatial changes . With the occurrence of frost, many animal activities are affected, and the honey bee, which is a cold-blooded insect, is affected by the surrounding temperature and reacts to this temperature. It should be kept in mind that the development of beekeeping has a close relationship with weather conditions and the time of moving colonies depends on this factor . In the annual climatic calendar of the growth of honey bee colonies, two active and inactive periods have been identified, and in the cold months of the year, the inactive periods start and special care is taken, however, there is a sharp decrease in the population and death of the colony. We are at the end of winter, which is one of the inhibiting factors for using bee pollination services and other products. The loss of the queen due to changes in environmental conditions such as: Temperature, high humidity and prolonged cold in mountainous areas and lack of food in hives are among the most common problems of bee breeding in very low temperatures).Winter deaths and reduction of bee colony population in cold regions, an important part of which is due to environmental and climatic conditions, increase the importance of studying this matter (Pettis et al., 2010). With the climate calendar in hand and the proper location of the apiaries in the cold months of the year by the beekeepers, we will see a significant reduction in losses, business improvement and more productivity. A lot of research has been done in the field of honey bee wintering all over the world, which shows the close relationship between the cold winter weather and the temperature of the investigated environment, and the result shows that the minimum consumption of honey in large colonies is in the temperature range of -10 and 10+ degrees Celsius in temperate regions. ). Researches show that in relation to minimum winter honey consumption of bee colonies, the temperature reaches 4 to 5 degrees Celsius. By examining the effects of climate changes on the population of colonies and their diseases, it was found that considering the climatic conditions plays an essential role in beekeeping management .The research conducted in relation to the effect of climate change on a micro scale and its impact on the migration conditions of colonies in high altitudes were investigated and an advanced monitoring system was proposed ). The effects of different times of the day, temperature, humidity and air pressure on the flight of various types of stingless bees were studied and the results showed that the flight activities of these types of bees are affected by atmospheric conditions and the elements of day length, heat, humidity and pressure.

Millet fodder plant is one of the important plants in Iran and the world, and due to its abundance of nutrients and its resistance to drought, it has a special advantage over other forages.The purpose of this research is to identify the areas prone to millet fodder cultivation in Ardabil province with multi-criteria methods and using the data of climatic elements and factors; Rainfall, average temperature, minimum temperature, maximum temperature, altitude, slope and soil depth.AHP, ANP, DEMATEL, Shannon Antropy and WLC methods were used to determine the weights of criteria and options.By using the weighted linear combination method in the GIS environment, information layers were integrated and the final map of millet fodder cultivation was prepared.The results showed that about 25% are very suitable, 36% are suitable, 30% are slightly suitable and 4.05% are unsuitable for millet fodder cultivation in Ardabil province.The results of AHP, ANP, DEMATE models showed that rainfall and temperature criteria, and in the Shannon Antropy model, height and slope have the most influence during the growth period of millet fodder.The output classification of two WLC and Antropy Shanon models about options showed that millet fodder cultivation areas overlap in both methods and the northern and central regions of the province have suitable conditions for millet fodder cultivation.

Today, fine dust and dust storms have become one of the important issues and problems of Iran and other regions of the world. This study is conducted to identify synoptic patterns of the dust storms in Ardabil Province (Iran) and monitor the origin and pathway of its places. The studied period is 34 years (1979-2013). The data used in this work are from synoptic stations of Ardabil province and the NASA’s upper atmosphere database. To achieve the goals of the study, the Environment to Circulation, Hierarchical Clustering Methods, and HYSPLIT model were used. According to the results, three patterns of geopotential height at 500 hPa levels were identified. Pattern No. 1 and 2 are almost similar to each other and represent the occurrence of a deep trough that formed from Central Europe and extended to the middle of the Red Sea. Based on these patterns, the study area is located in the East of this trough. The third pattern represents the occurrence of cut-of-low pressure blocking over the Black Sea and adjacent areas and placement of Ardabil province in the East trough of the formed blocking. The origin of dust in patterns 1 and 2 is the Eastern regions of Iraq and West of Iran while in pattern 3 is at 500 hPa level of the central areas of Iraq and at pressure levels of 850 and 1000 hPa of the central regions of Syria.

Assessment of agricultural crop potential areas based on potential climatic and natural talents plays an effective role in land use design and planning. Therefore, the present study aimed to evaluate the elements and factors affecting grape crop cultivation by multi-criteria decision making methods. Using data such as temperature (mean, minimum and maximum), rainfall, percentage of slope, elevation above sea level and soil depth data were used to evaluate and zonation of grape crops. In this research, hierarchical process (AHP), ARAS method and weighted linear combination method (WLC) were used to evaluate the effects of elements and climatic factors for cultivating grapes in Meshgin region. The results of the study showed that eastern and southern areas of Meshginshahr, Doostbeigloo and Moshiran, which are located in Gharehsoo River and downstream of other rivers, are suitable for growing grapes. The evaluation carried out by AHP method, land use, altitude, sunshine hours, rainfall and temperature among the studied criteria had the greatest effect on the cultivation of grapes in the region, respectively. According to the maps extracted from WLC method in GIS medium, about 34% of the area of Meshginshahr area is very suitable, 28% is suitable, 22% is slightly suitable and 16% is unsuitable for grape crop cultivation.

IntroductionHeat waves are one of the most dangerous climate threats associated with global warming, affecting society, economy and environment (Kogenhof et al., 2015: 930). We can say that the first step to control or at least reduce the damage caused by climatic hazards, including heat waves, is to define, detect and identify their characteristics using scientific methods (Abbasnia et al., 2016: 25). Therefore the purpose of this study is Simulation and prediction of maximum temperature and heat waves Southwest of Iran (Case study: Ahvaz and Ilam cities)MethodologyIn the present study to identify heat waves, Maximum daily temperature data of each studied stations, from 1961 to 2005, were obtained from the Meteorological Organization and SDSM software and CanESM2 model and three RCP scenarios (2.6, 4.5 and 8.5) were used. Then using error measurement indicators the lowest risk scenario was selected for each city and the maximum temperature was predicted based on that scenario and using the Fumiaki index and through programming in MATLAB software, Days that had temperatures above +2 standard deviation or above average (NTD) and these conditions lasted for at least two days, were identified and selected as the day with heat waves. The Fumiaki index is obtained by relation 1:(1 (T(i,j) ) ̅=∑_(n=2020)^2050▒〖T(i,j,n)÷N〗 Where T (i, j, n) temperature of day i th from month j th in year n th, (T (i,j)) ̅ the average temperature of day i from month j. To eliminate the noise in the mean, a 9-day moving average filter was performed on these data three times and calculated by the following equation (Fujibi et al., 2007; Ismail Nejad et al. 2014).(2 ∆T=(i,j,n)=T(i,j,n)-T(I,J)Where ∆T= (i, j, n) absolute deviation of temperature from the average on day j th of the month i th, in year n th compared to the average temperature of the same day. In order to the values of temperature deviation of different times and places to be comparable at a certain time and place, it is necessary to standardize these absolute values of temperature deviation by means of temperature diffraction. Like day-to-day changes, diffuse T∆ at 31 days for each day is calculated by the following equation:(3 (σ^2(i,j) ) ̅=∑_(n=2021)^2050▒〖 ∑_(j-31)^(j+31)▒〖[∆T(i,j^',n)-(∆T(i,j^',n) ) ̅ ]^2÷31N 〗〗 The value (T (i,j)) ̅ is the average temperature deviation in 31 days that is calculated by the following equation:(∆T*(i,j)) ̅=∑_(n=2020)^2050▒∑_(j=j-31)^(j+31)▒〖T(i,j^',n)÷31N 〗 (4Finally, (NTD) is calculated by the following equation:(5 (i,j,n)=∆T(i,j,n)÷(σ(i,j)) ̅ x Where .Then days with temperatures +2 above average (NTD) and lasting at least two days, were selected as the day with the HW. (Ismail Nejad et al, 2014). Equation 6:(6 2 ≥ NTD (i+p) NTD (i+p-1) ≥ 2, NTD (i-1), NTD (i+1)… NTD (i), To evaluate the ability of CanESM2 model scenarios to predict the average maximum temperature for the next 31 years, the outputs of each scenario are averaged by the absolute error values (MAD), mean square error (MSE), root mean square error (RMSE) were compared and the most accurate and least error scenario was selected. Equation 7-9.(7 MAD= (∑_(t=1)^n▒〖〖|A〗_t-F_t |〗)/n (8 MSE= (∑_(t=1)^n▒〖〖(A_t-F_t)〗^2 |〗)/n(9 RMSE=√((∑_(t=1)^n▒〖(A_t-F_t)〗^2 )/n) Results and discussionAccording to the results, during the next 31 years (2020-2020) there will be an increasing trend in the average maximum temperature in both Ahvaz and Ilam stations, which will be the most increasing trend in Ahvaz. Results also showed during the years 2050-2020, the heat waves of these two cities were identified and divided into two categories: short -term and Long-term waves. (Heat waves lasting between 2 to 5 days as short-term heat waves and waves lasting 6 days or more, long-term heat waves). According to the results, in both cities, 2-day heat waves will have the highest frequency, which is predicted to be higher in Ahvaz than in Ilam. But three-day waves in Ilam more than Ahvaz and 4-day heat wave in Ahvaz more and 5-day heat wave in both Ahvaz and Ilam only one case is predicted. The highest frequency of 2-day heat waves in Ahvaz cities in the months related to spring was predicted in Ilam in summer. The 3-day heat waves in both cities will be in the fall. Ahvaz four-day heat waves in autumn, in Ilam in summer. Five-day heat waves, one of which was forecast in the fall at both stations. The highest frequency of this hazard in both stations was related to 2-day warm waves, which were predicted more in Ahvaz than in Ilam, and in terms of time of occurrence in Ahvaz in late winter and early spring, and in Ilam in late summer and early autumn. Most heat waves will be experienced. In general, the occurrence of heat waves in the predicted period in both cities will often occur in the cold seasons of the year.ConclusionThe purpose of this study was to use the CanESM2 model in simulating and predicting the maximum temperature and heat waves of Ahvaz and Ilam cities as selected cities in southwest of Iran. Based on the results of simulation of maximum temperature and forecast of heat waves during the years 2020-2050. The maximum temperature in both stations will have an increasing trend, which will be the highest increasing trend in Ahvaz. The maximum continuity of heat waves in both stations will be 5 days and therefore short-term, and the 2-day heat wave will have the highest frequency. The trend of two-day heat waves in Ahvaz will be increasing and decreasing in Ilam, but the 3-day, 4, and 5-day waves did not show special trend in any of the stations. Over the next 31 years, heat waves will be less continuous and often occur in the cold months of the year.

The expansion of sustainable agriculture and the proper use of the country's water and soil resources require the selection of suitable plant species that are compatible with the climatic conditions of the country. Therefore, the optimal use of natural resources through the planting of plants compatible with the conditions of the region can guarantee human health, the sustainability and progress of sustainable agriculture, in fact, for the optimal use of land, the issues of water, soil and air cannot be analyzed separately For such researches, a framework such as zoning is proposed to plan, operate and properly use homogeneous pieces of land. Rosa damascene has a low water requirement and is highly adaptable to dry conditions. Considering Iran's climatic and geographical characteristics, the expansion of the cultivation of the Rosa damascene plant has gained double value.

Ardabil province in the north-west of Iran, with an area of 17,953 square kilometers, covers 1.09% of the total area of the country. Its geographical coordinates are between 37 degrees 25 minutes to 39 degrees 42 minutes north latitude and 47 degrees 3 minutes to 48 degrees 55 minutes east longitude. In the current research, using climatic criteria (Growth Degrree Days, annual precipitation, precipitation of the growing season, average temperature of the growing season, sunny hours of the growing season, and altitude) The growth of each plant starts from a certain thermal threshold, and the growth threshold of the rose is 2.5 degrees Celsius and the fuzzy TOPSIS method and the ANP network analysis process, the stations of Ardabil, Khalkhal, Parsabad and Meshginshahr have been selected for the cultivation Rosa damascene. The growth of each plant starts from a certain thermal threshold, and the growth threshold of the rose is 2.5 degrees Celsius. The steps of the TOPSIS technique include forming a decision matrix, forming a scale-free matrix, determining the Euclidean distance and choosing the best option, and the steps of the ANP method include creating a network structure between criteria, options and the goal, pairwise comparison of matrices and Formation of super matrix and selection It is the best option. In this model, each cluster and elements have a mutual relationship and the relationship of each criterion and clusters is checked with each other and they get a score between 1 and 9. The zoning and final drawing of the maps were done in the Surfer software environment and interpolation was done with the Radial Basis Functions method.

After weighting the effective parameters for the cultivation of Rosa damascene based on TOPSIS models and the ANP network analysis process and performing modeling and analysis of climate data, the final interpolation map for Rosa damascene cultivation was prepared based on the climatic potential and abilities. The results showed that in prioritizing the options for growing roses using the TOPSIS and ANP methods, the priority of the options is related to Meshgin Shahr, Khalkhal, Ardabil and Parsabad stations. In fact, the unrestricted lands include Meshgin Shahr station, which is the best place for cultivation due to its good climatic capabilities, and Ardabil and Khalkhal stations have low and medium restrictions for cultivation. The lands of this station have relatively weaker conditions than is the MeshginS hahr station , but good performance is expected from it. Parsabad station has very limited lands, which according to the assessment of climatic capability, this station lacks suitable potential for growing Rosa damascene.

In evaluating the ability of the habitat to plant a crop, not all criteria are equal. Some criteria play a key role. For this reason, factors are weighted in order to obtain a ranking of the value of decision criteria regarding suitable places for agriculture. The current research was conducted using TOPSIS and ANP methods and 6 effective atmospheric elements in the cultivation of Rosa damascene, standardization and formation of a ranking decision matrix based on these scores to determine and rank the Rosa damascene cultivation. These methods are more capable than other common methods. are doing the ranking more accurately. Finally, by interpolation (RBF) method, a map of the areas suitable for the cultivation of Rosa damascene was prepared. In the zoning map, there are very suitable areas for Mashgin Shahr station and unsuitable areas for cultivation at Parsabad station.

The sorghum forage plant with the scientific name Sorghum bicolor Moench belongs to the cereal family. This fodder is one of the most likely crop plants to drought stress and it has been called the camel of the crop plants of the world. Sorghum is considered a short-day plant and its suitable day length is 10 to 12 hours. Sorghum is resistant to dehydration and consumes 35-40% less water than corn during its growth period. You can grow it in the tropics all year round very sensitive about the spring cold. Length of forage growth period of sorghum based on climatic influence, environmental, agronomic and genotype factors has suggested at least 90 to more than 150 days in three main phases: vegetative, inflorescence development and seed growth. Also, it has specified the stages of development of sorghum as follows: stage zero; greening, observation of stalk pods on the soil surface. Step 1; View the third leaf collar. Step 2; View the fifth leaf collar. Step 3: Transition from vegetative to reproductive. Step 4 – Exit the flag leaf vertices. Step 5, Cluster Cover. Stage 6; 50 percent pollination. Step 7; Soft paste. Step 8; Stiff paste. Stage 9: Physiological Proceedings. The results showed that sorghum is cultivated at latitude between 45° of the northern hemisphere to 45° in the southern hemisphere, and in Philippines the height of sorghum is 1500 meters and in East Africa between 90 and 1500 m in East Africa, in America 25 to 850 m and in Africa from 400 m to 2500 m and generally cultivated from zero to 1500 m above sea level. Considering the importance of protein in the human diet, it is necessary to increase the production of fodder plants that are the source of animal protein production. In this research, an attempt is made to prepare suitable areas for the cultivation of sorghum fodder plant, which is very important for livestock feeding in Ardabil province, using the methods and criteria of the study of agricultural climate zoning map of sorghum fodder cultivation in Ardabil province.

Ardabil province is located in north-west of Iran and its location is at latitude of 37° and 45 minutes to 39° 42 minutes in the northern hemisphere and in geographical length of 47° and 3 minutes to 48° and 55 minutes of eastern longitude. Its area is about 17953 square kilometers (about 1.09% of the country's area). In this study, the optimum climatic requirement of sorghum forage cultivation from available sources was determined. Then, according to the favorable climatic requirement, precipitation, temperature, 12 synoptic stations during the statistical period (1400-2000) were obtained from Ardabil Meteorological Department and soil elevation, slope and depth maps were prepared from the relevant organizations. Also, multi-criteria decision making models, Shannon entropy, ANP and WLC weighted combined method and ARC GIS software, Export Choice and Super Decision software have been used for research. Shannon entropy model: It was introduced in 1972 by Shannon and Weaver. Shannon's entropy method works by saying that the greater the dispersion in a given index, the more important the index is (Shannon, 1988).Analytic Network Process (ANP):Network analysis is one of the multi-criteria decision making techniques and the developed form of analytical hierarchy process. This method is used to solve problems in which criteria and options are not independent of each other. In this process, measurement of relative values and significance such as analytic hierarchy process is done by paired comparison.Weighted Linear Composition (WLC):Weighted linear combination method is the most common technique in multi-criteria evaluation analysis. The purpose of multi-criteria assessment is to select the best option (alternative) based on their ranking through the evaluation of the main multi-criteria. This method is based on the concept of weighted average. Direct analysis and decision making based on the relative importance of the study gives weights to the criteria. The weighted combination method can be implemented using the geographic information system and the overlapping capabilities of this system. It is practical to use this method in both raster and vector GIS formats. After the final value of each option is determined, the options with the highest value will be the most suitable option for the intended purpose.

Shannon Entropy: In Shannon's entropy model, quantitative data collection is used by using questionnaires. In this model, five criteria: precipitation, temperature, elevation, slope and depth of soil were analyzed in seven stages. Data matrix formation was selected based on i option and j index. Then, the normalization of the data matrix numbers was done in order to perform other phases of Shannon's entropy model. The final ranking of the studied options for sorghum cultivation in Ardabil province was based on the studied criteria and after determining the importance factor of the indicators (WJ), the final prioritization of the options was formed by multiplication of the components of the group normalized decision matrix in the importance factor of indicators (WJ) Formation of priority coefficient matrix. Suitable options for sorghum cultivation compared to each index was formed. Finally, from the total row of priority coefficient of each option, the appropriate areas were formed for the Sorghum cultivation was estimated. The results showed that Bilehsavar and Parsabad regions with the degree of importance of 0.105 and 0.095 in terms of the studied criteria are in the appropriate condition for sorghum cultivation in Ardabil province. The results of data analysis based on the method WLC showed that the areas are suitable and very suitable for sorghum fodder cultivation in Ardabil province based on rainfall 49%, temperature 65%, altitude 52%, slope 44% and soil resistance 36%. The results of agricultural climate zoning of sorghum fodder cultivation in Ardabil province with WLC method in GIS environment showed that about 26% are very suitable, 34% are suitable, 35% are slightly suitable and 5% are unsuitable for sorghum fodder cultivation. Also, agricultural climate zoning with Shannon's entropy method showed that about 10% are very suitable, 19% are suitable, 59% are slightly suitable and 12% are unsuitable for sorghum cultivation in Ardabil province. Therefore, based on the methods studied at the level of Ardabil province, in case of water demand, tropical areas such as; Parsabad, Bileh Sowar, Dasht Givi and Ardabil are known to be suitable for sorghum cultivation.

Horizontal visibility is one of the most important optical characteristics of the atmosphere. Predicting horizontal visibility is of great importance in various aspects such as air pollution, air traffic, flight safety, road traffic, and maritime travel safety. The aim of the present study is to analyze the spatiotemporal variation of horizontal visibility in the southern coasts of the Caspian Sea. For this purpose, hourly data of horizontal visibility, present weather phenomenon, and relative humidity were used for a 70-year statistical period (1951-2020) in the study area. In this study, the extinction coefficient was calculated using the Koshmider formula. Finally, using the non-parametric Mann-Kendall test, the trend analysis of the frequency reduction of horizontal visibility phenomenon was conducted in the region. The results showed that among the studied stations, Babolsar, Ramsar, and Astara stations experienced an increasing trend, Nowshahr station experienced a decreasing trend, and Gonbad-e Kavus and Maraveh Tappeh stations had no trend in the extinction coefficient. Based on the Mann-Kendall output among the seasons, significant decreasing (increasing) trends were observed in the autumn and winter seasons, and no trend was observed in other time scales. The results of the analysis of the impact of weather parameters showed that among the factors affecting horizontal visibility, precipitation (39.75%) and dust (0.83%) had the highest and lowest percentage of impact, respectively, compared to other effective factors in the region. In general, it can be said that due to the forested nature and suitable vegetation cover in the region, the possibility of the occurrence of local dust storms is very low.

Sainfoin fodder plant is one of the fodder legumes, which is considered among fodder plants in terms of producing good, high-quality and acceptable fodder and competing with alfalfa fodder. Cultivation of this plant is not only compatible with cold regions, it is also established and cultivated well in tropical regions. A study of the morphological stages and evolution of Sainfoin fodder yield in spring season in (first China) showed that Sainfoin fodder has many species in 9 growth periods and is considered one of the most important pasture and crop fodder plants, and the place of its cultivation is the Iranian-Turanian region. In recent years, the development of Sainfoin fodder cultivation has been promoted with the combination of alfalfa fodder, which was effective in increasing the weight of livestock. Also, in Saskatchewan, Canada, in order to provide safe food for livestock, evaluation of Sainfoin and alfalfa fodder cultivation was carried out using rainfall and temperature, and the results showed that temperature and rainfall play an effective role during the growth period from germination to harvest of these fodder plants. The main goal of this research is the zoning of Sainfoin fodder cultivation in Ardabil province using effective criteria during the Sainfoin growth period. The difference between the present research and the studies conducted in this field is that more criteria and new data were used, as well as the efficiency of four methods during the growth period of Sainfoin fodder.

Ardabil province is located in the northwest of Iran, between latitude 37 degrees 45 minutes to 39 degrees 42 minutes and longitude 47 degrees 3 minutes to 48 degrees 55 minutes (Figure 1). This province with an area equal to 17953 square kilometers, the minimum and maximum altitude of the province is 32 meters in Parsabad and 4811 meters in Sablan, respectively. In this research, the data of precipitation, average temperature, minimum temperature and maximum temperature during the statistical period (1990 to 2020) and altitude, land slope and soil depth were used, as well as ARC GIS and Export Choice software for data analysis and analysis process methods. Hierarchy (AHP), TOPSIS model, Shannon entropy and weighted linear combination (WLC) method were used for weighting and zoning. Hierarchical analysis process method The first step in the hierarchical analysis process is to determine the importance coefficient of the criteria, sub-criteria and options in Sainfoin fodder cultivation. Export Choice software was used to analyze the criteria in the hierarchical process. After determining the relative weight of the criteria, the inconsistency coefficient is calculated. If this coefficient is less than or equal to 0.1, the consistency in the judgments is acceptable. Topsis method The TOPSIS multi-criteria analysis process is as follows. Formation of data matrix: It is calculated based on m criteria and n options. Shannon entropy method The main idea of this method is that the greater the dispersion in the values of an index, the more important that index is. The steps of this method are as follows. Forming the data matrix: First, a two-dimensional matrix of options and indicators is formed, and the value of each indicator in each option is estimated using official statistics and field studies. And the closer the value of dj is to zero, it indicates of Weighted Linear Combination (WLC) method This method is the most common technique in multi-criteria analysis based on the concept of weighted average, where the final value of each specific option and the options that have the highest weight will be the target. Equation (12) is used to evaluate each option or Ai: where Xij represents the i-th option in relation to the j-th criterion and Wj is the standardized weight of the j-th criterion, so that the sum of Wj is equal to one. The relative importance weight of each criterion is displayed. By determining the maximum value of Ai, the most priority option is selected. In addition to combining all parameters or layers, the WLC method also considers the importance of each parameter based on the weight given to that parameter. Table (2) shows the optimal climatic requirement of spruce fodder cultivation.

In this research, to locate Sainfoin fodder cultivation from the studied methods and also from the criteria; Precipitation, average temperature, minimum temperature, maximum temperature, altitude, slope and soil depth were used. The results showed that in all methods; Precipitation has the most important effect during the growth period of Sainfoin; Therefore, precipitation is the most limiting criterion in the cultivation of Sainfoin fodder in Ardabil province. The results of the weight criteria with AHP, TOPSIS, and Shannon's Antropy methods showed that precipitation, average temperature and minimum temperature with the highest weight are respectively the most important influencing parameters in Sainfoin fodder cultivation. Also, the results of combining the criteria with the WLC method in the GIS environment showed that the lands of Ardabil province have very suitable (29%), suitable (40%), slightly suitable (26%) and unsuitable (5%) for growing Sainfoin fodder(Fig,5). The results of the weighted value by AHP method showed that precipitation with a weighted criterion of 0.143, maximum temperature of 0.126 and average temperature of 0.089 among the studied parameters have the greatest effect on the growth stages of Sainfoin Finally, with the use of TOPSIS methods, about 5% and Shannon's entropy about 12% of the area of the province is very suitable for cultivating Sainfoin fodder; Therefore, compared to the studied methods in this research, the results showed that the weighted linear combination (WLC) method is the most suitable method for the zoning of Sainfoin in Ardabil province compared to the current situation. Therefore, the suitable areas for growing spruce fodder are located in the north and center of Ardabil province, which is due to the suitable climatic and topographical conditions. Therefore, the suitable areas

Urbanization changes natural landscapes to human-made spaces and uses. With the expansion of cities, many of these spaces give way to roads, buildings and urban facilities and cause changes in different levels of the city, and these changes have very important effects on weather conditions (Shamsipour et al. 2013: 59). )The development of urbanization is one of the effective factors in increasing the air temperature in urban areas, which causes the creation of thermal islands in these places compared to the surrounding environment. This factor can have a negative effect on air quality and endanger the general health of society. (Mousavi Baighi et al., 2010. 190). What is considered as a fundamental defect in monitoring the temperature of the earth's surface is the lack of sufficient meteorological stations to know the temperature values. Today, this shortcoming has been solved by remote sensing and it can cover a large area of the earth's surface.

The study area is Amol city. The city of Amol is located in the Mazandaran province and the sides of the Heraz River with a height of 76 meters above sea level at 52 degrees and 21 minutes east longitude and 36 degrees and 25 minutes north latitude and at a distance of 70 kilometers west of Sari, the capital of the province, 18 kilometers south of the Caspian Sea and 6 It is located one kilometer north of Alborz mountain and 180 kilometers northeast of Tehran.In this research, Landsat 8 satellite images and Landsat 5 satellite images were used for 1990 in order to extract the land use map and surface temperature of 2020. In order to remove the effect of cloud cover from the images as well as the high intensity of sunlight, the desired images were taken from the summer season. Google Earth software was used for better accuracy of images, ENVI 5.3 software was used for atmospheric and radiometric corrections, and finally ARC GIS 10.8 software was used to prepare relevant maps.Using the atmospheric correction model (FLAASH), the data were qualitatively controlled and the radiometric error of the satellite images was corrected. In order to obtain a statistical set that represents the spectral pattern of land cover, training data must be selected before supervised classification of images. At this stage, information from the uses and topographical maps of the region were prepared using the visual interpretation of the images for all five floors, to prepare educational data for use in supervised classification operations. Maximum likelihood classification method was used for land use classification. This method is considered a part of the supervised methods for classification and for this purpose it uses a set of training data. In this method, after evaluating the probabilities in each class, the pixels are assigned to the classes that have the most similarity, and if the probability values are lower than the introduced threshold, they are considered as unclassified pixels.After that, the brightness temperature of the sensor is done by converting the digital values of band 6 in Landsat 4 and 5 and also band 10 in Landsat 8 to spectral radiance and converting the spectral radiance to the brightness temperature of the sensor in terms of Kelvin.Then, red and near-infrared bands were used to calculate NDVI to obtain the normalized vegetation difference index. After calculating NDVI we need to get Emissivity. Emissivity is the amount of reflection of a phenomenon relative to the black body. Then the land surface temperature (LST) is calculated. By using LST, it is possible to calculate the temperatures near the surface of the earth. In order to know and evaluate the correctness and accuracy of the classification, the user's accuracy, overall accuracy and Kappa coefficient were calculated in 1990 and 2020.

In this research, in the first step, the classification and the resulting changes were done in a specific time frame in Amol city and its surroundings. The classification results indicate that the classification in both periods, especially in 2020, was highly accurate, and its kappa coefficient and overall accuracy were at their highest coefficient, i.e. 100.After classification, the changes obtained in the area were examined for a period of 30 years and the changes were extracted for each land use in terms of hectares. The change of use from agriculture to the city and also from the city to roads and streets have the most changes. These changes indicate that the increase in urban use has caused a decrease in agricultural use and the size of urban areas has increased.Using Landsat satellite images, the temperature of the earth's surface has been studied in relation to land use and the results showed that the temperature is different in different uses. The highest temperature recorded for the years 1990 and 2020 in Amol city is related to urban use, the recorded temperature of which is 32.6 and 40.5, respectively, which shows the concentration of heat in urban areas. Urban use has the highest temperature due to the presence of man-made factors and heat absorbers such as asphalt, concrete and the presence of machinery. Also, the presence of tall buildings acts as a barrier to the heat escaping to the surroundings and in some way traps the heat inside the cityWith the development of urbanization in Amel city, a significant part of the area of natural and forest areas has been replaced by industrial areas, buildings and other infrastructures. The lowest temperature recorded in Amol city is related to forest use with 23.8 and 28.4 degrees Celsius. In forest areas, due to high albedo, high humidity and more open space, the temperature is lower and heat absorption is low there.The relevant researchers and experts in the region can use the results of this research to obtain information about the temperature of the earth's surface, land use, and also the changes that have occurred in the region, In order to predict the future situation of the region, they will take appropriate and correct policies.

Today, climate issues threaten the security of the world, security which is considered necessary and vital in all fields and for all people. The phenomenon of climate change can affect the water requirement of crops by changing the amount of evaporation and transpiration of plants and the duration, intensity and time of rainfall. The studies related to climate change that have been conducted in Iran in recent years have focused more on climatic indicators and the effects of these changes on agricultural production have been given less attention. Therefore, assessing the effects of climate change on agriculture is an essential need. Due to the fact that Ardabil province is one of the poles of agriculture and animal husbandry and any change in the climate will endanger the lives of most of the residents of this region and will cause a change in the use of farms, pastures and the loss of agricultural production.kkkT Therefore, assessing the effects of climate

The study area is located on the slopes of Sabalan Mountain in Ardabil and East Azerbaijan provinces. Its geographical location is located at latitudes of 37 degrees and 44 minutes to 38 degrees 25 minutes and longitude 46 degrees and 22 minutes to 48 degrees 41 minutes. The minimum height of the area is 371 meters and its maximum is 4811 meters above sea level (Fig, 1). This study was conducted to influence climate change in wheat cultivation on slopes of Sabalan mountain. The important part of this research is based on statistics and information about meshkinshahr and sarab synoptic stations. In order to investigate the climate change conditions, a basic statistical period and a period as climate change should be determined. Therefore, statistical periods in this study from 1995 to 2015 and climate change period from 2016 to 2045 and 2046 were selected. Statistics about the studied stations were obtained from the Statistics and Information Bank of the National Meteorological Organization. The data taken from these statistics include: maximum and minimum temperature,daily rainfall and sunshine. to work with the LARS-WG model; First, the studied data should be sorted as Julius days. After collecting data in the Excel environment, it should be noted that there is no missing data, in case of missing, it must be encoded with -99. Aggregated data must be stored in a folder in nodpad with st extension.The address of folders stored in the N environment should be provided to the model from the option series, and the output data address should be given to the model. How to choose a scenario. First, in Excel environment, statistical data is placed in a column and in the next step, the generated data for each scenario is placed in the columns in front of each column of observational statistics, after preparing this step, the data is taken to the spss environment and correlation is taken between observational and production data. Production scenarios that are highly correlated with observational statistics are accepted as the studied scenario. CROPWAT software was used to estimate water requirement and effective precipitation. By entering minimum temperature, maximum temperature, relative humidity, wind speed and number of sunshine hours related to the plant, as well as the environment and region and its cultivation time, you can calculate the water requirement of the plant at different growth stages. Figure 2 shows the steps of data analysis in CROPWAT software.

In this study, first, the power of LARS-WG model for the basic statistical period of the years (1995-2015) was measured. The purpose of this assessment is whether the model has the ability to simulate for future periods. To do this, the tst file containing the results of comparing the statistical characteristics of the observed data with the simulated data was plotted as a diagram (Shapes, 2 and 3). The results showed that in Meshkinshahr station, the model has better efficiency for simulating maximum temperature and minimum temperature. The observed temperature and simulated temperature for 1995-2015 are similar and the diagrams are overlapping. Also, the deviation of production criteria is in the range of number one. This model is not effective in simulating the sunshine hour because it simulates the amount of sunshine hours in the first half of the year less than the actual size. In the case of rainfall, the model is better than April and May in other months. In Sarab station, the data were performed based on LARS-WG model by comparing the statistical period data and the produced data. To ensure the ability of computational data model, they were compared by model and observational data in the studied stations. Comparative results show the data of minimum temperature, maximum temperature, precipitation and sunshine in mirage synoptic stations for the base period. The capability of LARS-WG model in modeling minimum temperature, maximum temperature and radiation in these stations is completely in accordance with the observed data. The standard deviation rate is between 0.5 and 1. The results of this study show that in Meshkinshahr station, precipitation and temperature in the period 2016 to 2045 are -3.9 and +1.73, respectively, and these two variables in the period 2046 to 2065 are -6.67 and +1.80, respectively. In Sarab station, precipitation and temperature in the period 2016 to 2045 were +6.17 and -0.69, respectively, and in the statistical period of 2046 to 2065 were -12.91 and +0.37, respectively. As a result, rainfall in the coming periods is associated with a decrease in Sarab and Meshkinshahr stations, respectively. Temperatures are also rising at about 2 °C in Meshkinshahr station and the temperature increase is low in Sarab station. In comparison, Sarab plain has a wonderful state because by the period 2046 to 2065 the rainfall in this plain will decrease about 13% compared to the base period, in the same time period, wheat evapotranspiration will reach from 530 mm in the base period to 887 mm in the period 2046 to 2065. Wheat water requirement also increases from 422 mm in the base period to 810 mm, i.e. about 92%. Also, modeling shows that the average minimum temperature of this region decreases from -3 in the base period to -9.67 °C in January and from -4.3 to -8.23 in February. According to the modeling and with the decrease in rainfall in this region, wheat cultivation in this plain will face limitations in the future. However, the results of the models indicate that meshkinshahr plain is better in future periods than Sarab plain.

The alfalfa plant with the scientific name Medicago sativa L is considered the most important fodder plant in the world and it is a very high quality fodder suitable for all kinds of livestock (Kirimi, 2002). Alfalfa fodder plant is known as the queen of fodder plants in terms of nutritional value and palatability due to the variety of species compared to other fodder plants (Toran et al., 2017). In Iran, the area under alfalfa cultivation is 340,767 hectares and its production amount is 3,551,850 tons, and in Ardabil province, the area under alfalfa cultivation is 9,065 hectares and the annual production amount of alfalfa is 63,105 tons (Ministry of Jihad Agriculture, 2020). Examining weather data and their effect on plants is one of the most important factors in increasing productivity. Therefore, each area has potential and limitations regarding crop cultivation that is compatible with a specific climate, which studies the feasibility of suitable areas for cultivation. The main goal of this research is to locate alfalfa fodder cultivation in Ardabil province using water and meteorological criteria during alfalfa growth period. The difference between the present research and other studies in this field is that it studies the efficiency of four methods during the alfalfa fodder growth period.

Ardabil province is located in the northwest of Iran, and its location is in the latitude of 37 degrees and 45 minutes to 39 degrees and 42 minutes of north latitude and the geographical longitude of 47 degrees and 3 minutes to 48 degrees and 55 minutes of east longitude. In this research, from the data of annual precipitation, average annual temperature, minimum annual temperature and maximum annual temperature, six synoptic stations during the statistical period (1990 to 2020) and the height and slope of the land, as well as from the software; ARC GIS, Export Choice and Super Decision have been used. In order to weight and locate alfalfa crops, the methods of Analytical Hierarchy Process (AHP), Analytical Network Model (ANP), Fuzzy Hierarchical Process (FAHP) and Weighted Method (WLC) have been used.

In this research, alfalfa fodder cultivation location in Ardabil province was evaluated and investigated using AHP, FAHP, ANP and WLC methods. In the AHP method, the results with ExportChoice software analysis showed that annual precipitation with a weight of 0.377, average temperature with a weight of 0.258, and maximum temperature with a weight of 0.112 were respectively recognized as the most important criteria during the alfalfa growth period. The results of the FAHP method study showed that precipitation with a weight of 0.367, average temperature with a weight of 0.259, and minimum temperature with a weight of 0.105 are respectively effective in the stages of alfalfa fodder cultivation. In the ANP method with the analysis of Super Dicision software, the results showed that temperature criteria (average, minimum and maximum) with a weight of 0.404, annual precipitation with a weight of 0.289 and topography (height and slope) with a weight of 0.056 are the most important effective parameters, respectively. During the growth period, fodder is alfalfa. By combining the studied criteria during the growth period of alfalfa fodder with the WLC method in the GIS environment, the location of alfalfa cultivation in Ardabil province was done.

The final results of the data analysis with the studied methods showed that rainfall, temperature and topography criteria respectively play an important role during the alfalfa growth period and also by combining the data; A location map of alfalfa fodder cultivation in Ardabil province was prepared. About 22% is very suitable, 21% is suitable, 23% is slightly suitable and 24% is unsuitable for alfalfa cultivation and The results of network analysis (ANP) showed that; Pars Abad region with a score of 238/., Sablan and Meshkin Shahr area with a score of 226/. domain with a score of 228/. compared to other studied stations, they have priority for alfalfa cultivation. Therefore, it is suggested; A- Studies that are carried out with multi-criteria methods on agricultural products, their weighting should be done based on the study of the optimal climatic needs of that crop by the researcher, not through a questionnaire. B- Ardabil province is suitable for the cultivation of alfalfa fodder in terms of climatic conditions and place. It is recommended to grow alfalfa fodder instead of non-strategic crops that require a lot of water.

After apples and pears, the Quince tree is the most important fruit in the group of seed trees. Quince fruit has been of interest for a long time. In recent years, uniform planting of Quince fruit orchards has been developed in different provinces. Based on this, the zoning of Quince tree cultivation is required according to the climatic and environmental conditions. The purpose of this research is to identify the areas of Quince tree cultivation in Ardabil province with multi-criteria methods, using indicators; Rainfall, average temperature, minimum temperature, maximum temperature, height, slope and soil depth in the GIS environment. To determine the weight criteria of indicators and zoning of Quince tree agricultural climate, AHP, ANP, Shanon Entropy, DEMATEL and WLC methods were used that AHP, ANP and DEMATEL methods played the most important role in determining the weighted value of indices and Antropy Shanon and WLC methods in agricultural climate zoning. In general, the results of the methods analysis showed that; The average temperature and the maximum temperature are the most important indicators during the growth period of Quince tree in Ardabil province. But the indicators of rain, minimum temperature, height, slope and depth of soil in some areas of the province create restrictions for the cultivation of Quince tree. The results of climatic zoning methods indicate that; About 27% of the area of Ardabil province is very suitable, 31% is suitable, 20% is slightly suitable, and 22% is unsuitable for the cultivation of Quince tree. The northern areas of the province and the city limits of Givi and Khalkhal provinces are known as suitable areas for the cultivation of Quince tree based on the studied methods.

the statistics of the ECMWF database were used for the observation data of the two stations of Semiram and Urmia during a 21-year period (1996-20016).In order to investigate the effects of climate fluctuations, the daily data of dynamic micro-rotation of the CORDEX project was used for the output of the ICHEC-EC-EARTH model under the RCP8.5 and RCP4.5 radiative forcing (RCP) scenarios for the period (2017-2037). By using the data of the stations and the outputs of the micro scale model, and by using the perceptron neural network and linear regression, the performance was simulated. Then, to evaluate the efficiency of the models, R, R2, MSE, RMSE, and NRMSE statistics were used, and the non-parametric Menkendall test and age slope were used for the performance trend. The result of comparing the output of artificial neural networks with the linear regression model shows that the error rate of the neural network is less and the simulated results are close to the real observations to a very acceptable extent. The phenological stages, including bud blooming to fruit ripening in the stations under both scenarios, and in all the phenological stages in the future period will be completed earlier than the base period, and the length of the growth period will also decrease. The amount of future yield in Urmia station under RCP4.5 and RCP8.5 scenarios respectively yield 3.7 and 2.2 tons per hectare and in Semiram station yield 1.4 and 3 respectively tons per hectare will decrease. The results show that in the future in the study areas, with the change in the time of occurrence of the length of the growth period, all the phenological stages as well as the declining performance of apple trees will be subject to climatic fluctuations

It is necessary to know the potential abilities and the functioning of the environmental factors affecting beekeeping, such as the identification of plant species and the length of the flowering period of plants, considering the role and importance of weather elements. With this information in hand, a fundamental step can be taken in the optimal use of honey bee food resources and the establishment of colonies in the right place and time. In this research, due to the great importance of temperature in bee breeding, 20 years of daily temperature statistics of meteorological stations were used. These data were used to identify the optimal temperature thresholds for honey bees and were made into a zoned map with the geographic information system. By using the degree index of growth days and regression equations of flowering dates to determine the migration time of the colonies, the evaluation and the results showed that the temperature thresholds of 10 and 20 degrees Celsius from May to September are among the active temperatures and to take advantage of the thermal potential of the region and the thermal power in the direction Optimum, special reference should be made to the months of June and July, which have the right temperature and the time when the plants of the Sablan area begin to flower, the difference in altitude is also very important in terms of temperature, because it causes the colonies to move at different temperatures. The results show that the oregano plant has a higher growth and flowering area than other plants in the region, so that it covers a large area in all stations from the middle of June and is a good source of food for honeybees in the hot months of the year. Finally, it should be added that by using the obtained calendar for the warm half of the year, the status of establishing the colonies in the right place and time will increase the per capita production and more income for the beekeepers.

Flood as a natural disaster with the highest relative frequency of occurrence has always threatened human life. The purpose of this study was discovering the relationship between atmospheric circulation patterns and floods in the Balikhlochai watershed of Ardabil in order to prevent its dangers with an environmental approach to circulation. For this purpose, discharge data for three stations of Almas, Nir, and Gilandeh from the period 2009-2017 were obtained from the regional water department of Ardabil province. Using the ward hierarchical clustering method, two floods occurred on March 7, 2010 and December 8, 2010 were selected and analyzed. The data related to the upper levels of the atmosphere were obtained from the National Center for Environmental Prediction (NCEP-NCAR) website and combined maps of sea level pressure with geopotential height of 500 hectopascals, wind vector with precipitable water, omega with tawai and half-molar specific humidity in Gardes software were drawn. The results of the synoptic analysis showed that the dominance of the Mediterranean thermal low pressure system and the Chinese thermal high pressure system were important factors in the atmospheric disturbance, and besides that, the location of the studied area in front of the landing axis of the Eastern Mediterranean fleet resulted in rotating air movements. And the vertical air velocity of the studied area showed an unstable atmosphere. The specific humidity has also increased since the day before the flood in the lower layers of the atmosphere, and the flow of moisture from the Mediterranean Sea through the western subtropical winds on the atmosphere of the studied area has played an important role in causing torrential rains.

Snow as a climatic element due to the rainy season, its solidity, the area covered and the consequences it brings, deserves the study and attention of researchers and users of the environment. It has played a major and fundamental role, and in terms of microclimate, due to its weak heat conduction, it is considered a good protection for its vegetation against the cold (Kaviani, 2010). In the generally dry and semi-arid land of Iran, snowfall and snowy days have a great value, among which the amount of snowfall, the number of days of occurrence, its ratio with the days of precipitation, during the period of descent and its beneficial and harmful consequences, each of them can be the subject of There should be separate researches, while the average number of rainy days in Iran ranges from less than 10 to about 115 days, the maximum number of snowy days is on average in the northwest region and about 25 days a year (Alijani, 2016). On the other hand, the effects of heavy snowfall and avalanches, the destruction of rural homes, the disruption of road transport, communications, daily activities, and many other consequences on the natural and human environment have attracted the attention of some researchers. It is true that some of these researches have been in the field of temporal changes of snowfall in recent decades. Due to the fact that studying and knowing the factors disturbing human peace and well-being seems to be necessary and knowing the changes in the trend and factors that generate the atmosphere of natural phenomena can be a way forward, so in this study, the aim is to analyze the heavy snowfall in Ardabil from a synoptic point of view. And to investigate the trend of changes in the frequency of snowy days with non-parametric methods.

This research has been carried out in order to investigate the synoptic heavy snowfall in Ardabil city with an environmental approach to circulation and to investigate the trend of changes in snowy days with non-parametric methods. In this regard, first the data related to the daily snowfall parameter for Ardabil synoptic station was received from the General Meteorological Department. Nonparametric Mann-Kendall method and sense estimator were used to analyze the time series trend of this variable.Mann-Kendall test In the Mann-Kendall test, the assumption of zero indicates randomness and the absence of a trend in the data series, and accepting the assumption of one indicates the presence of a trend in the data series. This test was first presented by Mann (1945) and then expanded by Kendall (1975) based on the rank of data in a time series and is calculated in two ways: 1- Statistical test (T) I-Kendall 2- Graphical test I- Kendall The calculation steps of this test are as follows (Zinali, 2015: 90).Sense Estimator test The sense estimator method, like the Mann-Kendall method, uses the difference analysis of observations of a time series. This method is based on calculating a median slope for the time series and judging the significance of the obtained slope at different confidence levels, and the steps to do it are as follows (Hajam et al., 1387: 161).

The purpose of this research is the synoptic investigation of heavy snowfall from an environmental perspective and investigating the trend of changes in snowy days with non-parametric methods in Ardabil. The results of the non-parametric Mann-Kendall test and sense estimator showed that the Test z value was -2.30 and the Qmed value was -0.931 at the confidence level of 95% and indicated a negative, downward and significant trend. Also, according to the results According to the analysis of satellite maps in the event of heavy snow on January 26, 1400, it was found that there are two high-pressure systems in the east and west of Iran, with their outward movement, they lead the nearby air mass towards the studied area, and the dominance of the high-pressure systems of Central Europe over the studied area. The study has caused the formation of weather conditions and has led to the stability of the air and its subsidence. This system has played a very prominent role in the transfer of cold air in the northern latitudes, and in addition, in the western part of Iran, it has formed a trough of atmospheric conditions in such a way that before the axis of the trough, the convective strengthening in the upper levels of the atmosphere leads the flow of cold northern winds to the lower latitudes. And especially the west of Iran. Due to the location of the studied area in the front part of the landing axis of the ship and the strengthening of the divergence in Wardspahr, the values of Tavai have become positive and the weather condition has become unstable. The movement of the westerly winds in the aforementioned nave channel has caused the moisture of the Black Sea and the Mediterranean Sea and its flow towards the studied area. On the other hand, the intensification of the wind speed up to 35 meters per second in the atmosphere of the studied area has fueled atmospheric disturbances, as well as the influx of cold currents. North, a cold air mass has condensed in the Naveh axis in the northwest of Iran and has lowered the surface temperature of the studied area to -2 degrees Celsius. The rule of cold air over the northwestern part of Iran has also reduced the thickness of the atmosphere and caused the contraction of the atmosphere. The results of this research are also aligned with the results of other researchers, such as Saleh and Eskandari (2012) and Dargahian and Alijani (2016), pointing to the role of deep troughs in the northwest of Iran, which play a very important role in the transfer of cold air from northern latitudes towards Iran. had. Also, Emininia et al. (2009), in the study of changes in heavy snowfall in the northwestern region of the country, pointed out that heavy snowfall in all stations and during the common statistical period had high fluctuations and a decreasing trend.

In urban regions, thermal islands are exacerbated by the heat waves (HWS) effect, and it has the potential to negatively influence the health and welfare of urban residents. Scientists predict that heat waves will intensify and become more persistent in the coming years due to climate change. As a result, the likelihood of these two phenomena occurring simultaneously will increase in the coming years, even in small, non-industrial cities. Therefore, the purpose of this study is to compare the impact rate of thermal islands from the occurrence of heat waves in Kermanshah and Ilam cities from 2003 to 2018 and It is tried to determine under the conditions of heat waves, Which of the studied cities and at what time of the day the intensity of urban heat islands has increased?

 In order to identify and extract heat waves, the maximum daily temperature data of Kermanshah and Iilam stations, from 2003 to 2018, by using Fumiaki Index and MATLAB software, days whit temperature above +2 standard deviation or above the mean Normalized Thermal Deviation (NTD) that lasted at least two days, were identified as the day with HWs and calculated by equation 1:                                                                                                                                                                     (1)
Where T (i, j, n) temperature of day i th from month j th in year n th,  the average temperature of day i from month j. To eliminate the noise in the mean, a 9-day moving average filter was performed on these data three times and calculated by equation 2:                                                                                                                                                                 (2)
Where ∆T= (i, j, n) absolute deviation of temperature from the long-term average on day j th of the month i th, in year n th compared to the long-term average temperature of the same day. In order to the values of temperature deviation of different times and places to be comparable at a certain time and place, it is necessary to standardize these absolute values of temperature deviation by means of temperature diffraction. Like day-to-day changes, diffuse T∆ at 31 days for each day is calculated by equation 3, then the 9-day moving average was performed three times
                                                                                                                                                           (3)
The value  is the average temperature deviation in 31 days that is calculated by equation 4:                                                                                                                                                          (4)
Finally, Normalized Thermal Deviation (NTD) is calculated by the following equation:                                                                                                                                                        (5)
Where .Then in MATLAB software, days with temperatures +2 above average (NTD) and lasting at least two days, were selected as the day with the HW (Equation 6).
                                                                                                                                                             (6)
Then the thermal island was calculated in Kermanshah and Iilam cities using Equation 7:                                                                                                                                                              (7)
Where SUHI, is the surface heat island, MLSTurban is the average surface temperature in the urban area and FLSTrural is the surface temperature with the highest frequency of occurrence in the rural area.

The purpose of this study was Comparison the Impact rate of thermal islands from the occurrence of heat waves in Kermanshah and Ilam cities. Which has had an increasing trend in Kermanshah and no trend in Ilam. Also, the highest monthly frequency of heat waves in both cities was in March. Also the maximum duration of this risk was 4 days and short-term in Kermanshah and 6 days and long-term in Ilam. The results also showed that in both the heat wave and no heat wave condition, most of the day the cold island and at night sometimes the heat island (although weak) is formed in the Kermanshah and Ilam city centers, but in the heat wave conditions, especially in daytime and in Kermanshah city, the intensity of thermal islands was higher than normal. Studies also showed that the persistence of heat waves did not play a significant role in the intensification of thermal islands because the impact of thermal islands from the occurrence of two-day and four-day heat waves was almost the same. In the studied cities, in both Heat wave and no heat wave condition, a cold island has been formed in the city center, but in each heat wave, the intensity of the cold island has been more than a normal day for at least one day. In Ilam, even at night, mostly the cold islands have been created in the city center, although its intensity has been less compared to the daily cold islands. However, the most intense heat island in Kermanshah was in normal conditions, which was 3.5 degrees Celsius, but in Ilam, the most intense heat island occurred in heat wave conditions, which was 1.6 degrees Celsius. According to the explanations provided, the occurrence of heat waves did not have an effect on the intensification of thermal islands, especially during the day. In heat wave condition, in both cities the percentage of relative humidity was lower than normal, but the maximum wind speed in both cities was sometimes higher than normal days. to some extent indicates the open development horizons of the progress of the study area.

According to the results, thermal islands in both cities, especially in the daytime, even in the absence of heat waves in the center of the cities under study and have been affected by the occurrence of heat waves. Therefore, because according to scientists, climate change will increase climate risks such as heat waves, and the current small and non-industrial cities will experience more heat waves in the coming years, and will certainly grow and develop. Therefore, in order to prevent the negative consequences of the interaction of heat waves and heat islands in the future, further research is necessary. Also, in order to reduce the intensity of thermal islands and reduce the surface temperature in the center of these cities in the coming years, solutions such as: covering surfaces and buildings with materials with high heat capacity, protection of green spaces and creating green roofs, especially in urban centers, paying attention to the direction of the wind in the constructions so that there is a possibility of wind canalization and heat discharge between the buildings. Adjusting the density of buildings and their decentralized construction in the center of these cities seems necessary.

Understanding the conditions for the onset and end of glaciers is essential because of their importance in agriculture, transportation, and environmental issues to reduce damage. Meshginshahr country due to geographical location, topography and location in the path of migratory air masses, often witnesses the occurrence of frost and damage caused by these climatic elements.The severe dependence of the economy of the people of this region on agriculture necessitates a careful study of the beginning and end dates of this devastating phenomemenon. In this research, by considering the temperature of zero and below zero Celsius degrees, the start and end dates of glaciation in Meshginshahr city during the statistical period 2000-2019 have been extracted and classified. In order to better understand the contents, these dates have been adapted into the Julian calendar. The return period of each of the mentioned glaciers by SMADA software with a probability of 2, 3, 5, 10, 25, 50, 100 and 200 percent was calculated and the most appropriate statistical distribution was selected to survey the freezing. Finally, by extracting the synoptic maps related to the days of frost occurrence on the earth's surface, iso-altitude of 500 hPa, wind vector and temperature of the middle layers of the atmosphere, thickness of the atmosphere and level of 500 hPa, it was determined that the occurrence of frost on the earth's surface is related to the expansion of the high-pressure tongue of the migrant of Northern Europe and The central one is the high pressures of the North Caspian barrier and the expansion of the Siberian transect tongue. The level height of 500 hectopascals is also due to the placement in front and back of the western winds, and the maps of Tawai show the descent of the air mass most of the time. The results of this research indicate that in Meshginshahr city, the trend of autumn frosts is relatively stable and with a gentle slope towards the cold months of the year and spring frosts is moving towards the warm months of the year. IntroductionAccording to the time of occurrence, frost can be divided into two types: early and late. In the autumn season, the frost earlier than the usual time is called early frost, and in the spring season, the occurrence of frost later than the usual time is called late frost. These types of frosts affect the phenological stages of crops more than anything else, and every year they cause a lot of damage to farmers and gardeners due to frost damage to their crops (Hejazizadeh and Moghimi, 1386: 88). Therefore, the study of this period of the year, which is called the glacial period, in terms of its beginning and end, can be of great help to the officials of economic, civil, or even agricultural affairs and its planners, in such a way that some of their activities that are affected by this period Adjust it so that they don't get into trouble and crisis. On the other hand, the results of this research can help executive officials in planning for the sustainable development of the country and province. For this purpose, many foreign and domestic studies have been conducted in this field, including Idalo Gualuz et al. (2017), by investigating the causes of climate change in Spain, they investigated the effect of late spring frosts on the flowering phenology of trees. The results of the investigations show an increase in the minimum temperature in all weather stations compared to the base period. Meshkinshahr city, due to its location in the path of high-pressure migrants and cold fronts, mostly faces the phenomenon of frost in the spring and autumn seasons, and enough time is needed to harvest garden crops in the autumn season, and in the spring season, due to the regrowth of plants and Blooming of fruits should be provided in such a way that no damages are caused to the products. On the other hand, the transport sector of the studied area is the road connecting the province center to the cities of Garmi, Beile Sawar and Dasht Moghan, and the study of early and late frosts in the region is necessary to avoid damage to the economic sector of the province Methodology After obtaining the required minimum daily temperature statistics for the mentioned years from Meshkinshahr meteorological station, it is necessary to determine the date of the first and last frost for the study and statistical analysis of each year. The method of obtaining these dates is that from the first of October of the solar year, the temperature was checked at least daily, and the temperature that reached the threshold of zero and below zero degrees Celsius was considered as the date of the first early autumn frost. Also, to determine the date of the last spring frost, from the end of spring, the minimum daily control temperature and the last day when the temperature was equal to zero or below zero were considered as the date of the last spring frost. Statistical information and data were calculated and analyzed using EXCEL (SPSS) software. In the following, the linear regression method (simple linear and polynomial) was used to analyze the change process of the mentioned glaciers. ) by drawing the polynomial trend on the ice time series, the increasing or decreasing periods of the ice can be studied during the time. SMADA software was used to calculate the return period of the mentioned frosts, and the return period of frosts is 50, 66.7, 80, 90, 96, 98, 99, and 99.5 percent with the return period of 2, 3, 5, 10, 25 percent. 50, 100, 200 years were determined. Then the type of ice, both radiation and advection, was determined. Finally, for the purpose of synoptic analysis of the start and end dates of the autumn and spring frosts of the region under study, the maps of the earth's surface, the iso-elevation of the 500 hpa level, the wind vector (in a combined form), the surface temperature of 500 hpa and the thickness of the atmosphere (difference between the surface height of 500 and 1000 hPa) combined form) and finally the 500 hectopascal level maps were extracted from Grads software and analyzed.

Societal needs elicit focus to new water sources including water extraction and developing adaptation to indigenous, climatic, economic and social conditions. The initial step in developing water extraction from humidity was determining optimal extraction areas with appropriate conditions. For this purpose, humidity and temperature criteria were collected utilizing satellite imagery which included soil type, surface wind speed, and 50 cm deep soil temperature data. Subsequently, criterion was mapped out based upon the role and importance of each factor obtained using hierarchical analysis in a GIS v10.2 environment. Employing linear phase functions, the information layer was phased and layers were subsequently combined using the 0.9 gamma phases function. Resultant findings of water extraction from humidity utilizing a condensing system revealed ~13.1 percent of Sistan and Baluchestan southern provinces (along Makran and Chabahar coasts), and its western Deligan region laid in very appropriate and appropriate areas. Conversely, about 83.9 percent of northern and eastern province areas were determined to lay in inappropriate extraction areas.

Tourism is one of the largest and high-yielding economic activity in the world, the development of which requires sufficient knowledge of the issues and economic factors, Social and cultural development in each region. One of the city's tourist areas in Khalkhal in Ardebil province, due to topographical and geological structure, is full of tourist sites in terms of ecotourism.

This research uses SWOT model and descriptive-analytical approach and field studies and libraries whose purpose is to assess the tourism potentials of Khalkhal city in Ardabil province.

Analysis of the above model in this study shows that in the matrix analysis, strengths are 1.61, weaknesses are 1.26, opportunities are equal to 1.77 and the amount of threat is equal to 1.19, tourism potentials of Khalkhal city, in the first priority aggressive strategies are the second priority in planning competitive strategies. For this purpose, first the initial strategies of SO with a value of 3.38 and then the strategies of OW with a value of 3.03 in the SWOT matrix are in the first and second priority, indicating the best strategies in sustainable tourism in Khalkhal region.

According to the results of the present study defensive strategies (WT) with a score of 2.45, conservative strategies (TS) with a score of 2.8, represents the weakest sustainable tourism strategy in the area known Khalkhal.

Heatwaves are one of the most harmful weather hazards to humans and the environment. The purpose of this study was to investigate the effect of heat waves on the heat islands of Tabriz metropolis during the years 2003-2008. For this purpose, maximum temperature data of Tabriz Synoptic Station were obtained from the Meteorological Organization and days with heatwaves were determined using Fumiaki index and MATLAB software. To investigate the effect of heatwaves on the intensification of thermal islands, warm waves in the hot and cold months of the year are selected and thermal islands for those days and a day without heatwaves with the lowest maximum temperature before each heatwave during the day and night at Modis Aqua were calculated. According to the results, the maximum heatwave constant was 4 days and had an increasing trend. Its highest frequency was in 2010 and in April, June, and December. According to the findings, in both hot and cold months, the intensity of the cold island of the day is often weak in both heatwave and no heatwave conditions, and with the occurrence of heatwaves, sometimes even the heat island in the city center has been created. At night time, at the same time as the heat waves, the heat island is often more intense than on normal days. Wind speed and relative humidity were lower than normal conditions in hot months compared to cold months. In the cold months, the cold island is often intensified by the heatwave both during the day and at night, compared to the normal day, but the heat island is weaker.