مطالعات جغرافیایی مناطق خشک

مطالعات جغرافیایی مناطق خشک

ارزیابی و مدلسازی تغییرات فیزیکی تالاب ارژن در رابطه با پارامترهای اقلیمی با استفاده از سنجش از دور

نوع مقاله : مقاله پژوهشی

نویسندگان
1 دانشگاه حکیم سبزواری
2 مرکز آموزش عالی فیروزآباد
چکیده
تغییرات شدید آب و هوایی، کاهش نزولات آسمانی، افزایش دما و به دنبال آن افزایش تبخیروتعرق در دهه­‌های اخیر باعث کاهش چشمگیر مساحت سطوح آبی شده است. در این بین، بررسی نوسان­‌های سطح آب دریاچه­‌ها، به منظور حفاظت آن‌ها به لحاظ اهمیت، ماهیت در سال­‌های اخیر در بین کشورها در سطح ملی و منطقه­‌ای جایگاه ویژه‌­ای پیدا کرده است. هدف از این پژوهش بررسی تغییرات فیزیکی تالاب ارژن و روند پارامترهای اقلیمی و نیز ارتباط بین موارد یاد شده است. جهت نیل به هدف یاد شده، با استفاده از تصاویر ماهواره لندست و محاسبه شاخص NDWI مساحت دریاچه‌­ها از سال ۱۹۸۶ تا ۲۰۱۸ محاسبه گردید. نتایج حاکی از کاهش مساحت در بازه­ی زمانی موردمطالعه است. به طوری که تالاب ارژن از سال ۲۰۱۳ به صورت کامل خشک شده است. کمترین میزان بارش ثبت شده در این بازه در سال­‌های ۲۰۰۸ و ۲۰۱۰ به ترتیب با میزان ۱۲۷/۸۲ و ۱۰۶/۷۶ میلی‌متر است. میانگین دمایی در دوره مطالعاتی ۲۰۱۸-۱۹۸۶، ۱۹/۴۴ درجه سانتی‌گراد بوده و دما در این بازه با میزان ۰/۶ درجه سانتی‌گراد روند افزایشی را طی کرده است. در بین پارامترهای آب و هوایی مورد بررسی پارامتر بارش با ضریب همبستگی حدود ۰/۵۳ و تبخیر و تعرق پتانسیل با ضریب همبستگی حدود ۰/۴۳- همبستگی بیش‌تری با تغییرات مساحت دریاچه‌­ها داشتند. جهت پیش‌­نگری پارامترهای اقلیمی دما و بارش منطقه مورد مطالعه در دهه‌­های آتی (۲۰۲۰-۲۰۵۰)  از مدل HadCM2 پروژه Cordex-WAS تحت دو سناریو RCP4.5 و RCP8.5 استفاده شد که نتایج بیانگر روند کاهشی بارش و افزایش دما است. از میان عوامل مورد بررسی در این پژوهش دو عامل اصلی، متوسط بارندگی سالیانه منطقه مورد مطالعه و تبخیر سالیانه در سال­‌های اخیر به عنوان عواملی که بیش‌ترین تأثیر و همبستگی را با تغییرات فیزیکی تالاب داشتند، مدنظر قرار گرفته شد.
کلیدواژه‌ها

عنوان مقاله English

Evaluation and modeling of physical changes in Arjan wetland in relation to climatic parameters using remote sensing

نویسندگان English

Rahman Zandi 1
Abouzar Nasiri 2
maryam khosravian 2
mahdi zarei 1
چکیده English

Severe climate change, declining rainfall, rising temperatures, and subsequent increased evapotranspiration have led to significant reductions in water levels in recent decades. In the meantime, the study of fluctuations in the water level of lakes, in order to protect them in terms of importance, has gained a special place in recent years among countries at the national and regional levels. The purpose of this study is to investigate the physical changes of Arjan wetland and the trend of climatic parameters as well as the relationship between the mentioned cases. To achieve this goal, the area of ​​the lakes from 1986 to 2018 was calculated using Landsat satellite images and the NDWI index. The results indicate a reduction in area over the period under study. It has been dried so that Arjan wetland has been completely since 2013. It is the lowest amount of precipitation recorded in this period in 2008 and 2010 with the amount of 127.82 and 107.7 mm, respectively. The average temperature in the study period 2018-1986 was 19.44 degrees Celsius and the temperature in this period has increased by 0.6 degrees Celsius. Among the studied climatic parameters, the precipitation parameter with a correlation coefficient of about 0.53 and the potential evapotranspiration with a correlation coefficient of about -0.43 were more correlated with changes in the area of ​​lakes. The HadCM2 model of Cordex-WAS project under two scenarios of RCP4.5 and RCP8.5 was used to predict the climatic parameters of temperature and precipitation of the study area in the coming decades (2020-2050). The results show a decreasing trend of precipitation. And rising temperatures. Among the factors studied in this study, two main factors, the average annual rainfall of the study area and annual evaporation in recent years were considered as the factors that had the greatest impact and correlation with the physical changes of the wetland.

کلیدواژه‌ها English

Physical changes
argan
climatic parameters
remote sensing
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دوره 13، شماره 49
پاییز 1401
صفحه 17-1

  • تاریخ دریافت 29 دی 1400
  • تاریخ بازنگری 29 بهمن 1400
  • تاریخ پذیرش 03 خرداد 1401
  • تاریخ انتشار 01 آذر 1401