ارزیابی مکانی روند دمای سطح زمین در اقلیمهای خراسان رضوی با سنجنده آکوا (از 2003 الی 2023)
مهندسی عمران فردوسی
مقاله 1 ، دوره 37، شماره 3 - شماره پیاپی 47 ، مهر 1403، صفحه 1-12 اصل مقاله (1.48 M )
نوع مقاله: مقاله پژوهشی
شناسه دیجیتال (DOI): 10.22067/jfcei.2024.88361.1302
نویسندگان
مجتبی گلدانی 1 ؛ حسین اعتمادفرد* 1 ؛ علی رضایی 2
1 گروه مهندسی عمران، دانشکده مهندسی، دانشگاه فردوسی مشهد، مشهد، ایران.
2 گروه علوم و مهندسی آب، دانشکده کشاورزی، دانشگاه فردوسی مشهد، مشهد، ایران.
چکیده
صنعتیشدن و افزایش مصرف سوختهای فسیلی گرمایش زمین را در پی داشته و موجب تغییر در طبیعت، اقلیم و زیست انسان شده است. مطالعه و پایش بلندمدت پارامترهای مرتبط با گرمایش زمین بهخصوص دمای سطح زمین با استفاده از تکنولوژیهایی مانند سنجشازدور میتواند به درک درست و بهتر این پدیده کمک کند. انرژی خورشید در طول روز به سطح زمین رسیده و دمای آن را افزایش میدهد، اما در طول شب رفتهرفته از آن خارج شده و دمای آن کاهش مییابد. در این تحقیق، به کمک سنجنده آکوا از مأموریت مودیس، تصاویر مربوط به شاخص LST در یک دوره ۲۰ساله از سال 2003 الی 2023 از استان خراسان رضوی واقع در شمال شرق ایران جمعآوری و بهصورت هفتگی میانگینگیری گردیدند. سپس به کمک رگرسیون خطی روند دمای سطح در منطقه در تمامی اقلیمها محاسبه شد. نتایج نشان میدهد که بهطورکلی شاخص LST در روز و شب افزایشی بوده؛ ولی در روز هنگام دمای سطح زمین افزایش بیشتری نسبت به مقدار آن در طول شب داشته است. دو اقلیم خشک و نیمهخشک در استان غالب هستند و میانگین افزایش دمای سطح برای آنها در روز هنگام به ترتیب 80/0 و 07/1 سانتیگراد بر دهه و شبهنگام 55/0 و 59/ سانتیگراد بر دهه بود. علاوه بر این، مشاهده شد ارتباط محسوسی بین اقلیمها و روند دمای سطح وجود ندارد و روند LST روز هنگام در مناطقی که دارای کاربری کشاورزی هستند کاهشی بوده اما روند LST شبهنگام ارتباطی به کاربری کشاورزی یا پوشش گیاهی نداشته است.
کلیدواژهها
آکوا ؛ اقلیم ؛ خراسان رضوی ؛ دمای سطح زمین ؛ مودیس
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