ارزیابی انواع الگوریتم های پنجره مجزاء برای محاسبه دمای سطح زمین جهت تعیین بهترین الگوریتم برای تصاویر سنجنده مودیس
الموضوعات :محمد کاظمی قراجه 1 , بهنام سلمانی 2 , بختیار فیضی زاده 3
1 - کارشناسی ارشد سنجش از دور و سیستم اطلاعات جغرافیایی، دانشکده برنامهریزی و علوم محیطی، دانشگاه تبریز، تبریز، ایران
2 - کارشناسی ارشد سنجش از دور و سیستم اطلاعات جغرافیایی، دانشکده برنامهریزی و علوم محیطی، دانشگاه تبریز، تبریز، ایران
3 - دانشیار گروه سنجش از دور و سیستم اطلاعات جغرافیایی، دانشکده برنامهریزی و علوم محیطی ، دانشگاه تبریز ، تبریز، ایران
الکلمات المفتاحية: الگوریتم های پنجره مجزاء (SW), دمای سطح زمین(LST), استان آذربایجان شرقی, سنجنده مودیس,
ملخص المقالة :
پیشینه و هدف در سال های اخیر مطالعه تغییرات اقلیمی و همچنین تاثیرات آن ها تبدیل به یک موضوع ثابت در عرصه های علمی بسیاری از کشورها شده است. یکی ازویژگی های اصلی این تغییرات، افزایش دمای هوا در طی 5 دهه اخیر نسبت به 500 سال گذشته است. به طوری که آمارها بیانگر افزایش یک درجه سانتی گراد در دمای هوا در طی 5 دهه اخیر هستند. به دمای تابشی پوسته زمین و به مقدار خالص انرژی که تحت شرایط اقلیمی درسطح زمین به توازن رسیده و به مقدار انرژی رسیده، گسیلمندی سطح، رطوبت و جریان هوای اتمسفر بستگی دارد، دمای سطح زمین می گویند. دمای سطح زمین به عنوان یکی از متغیرهای کلیدی در مطالعات اقلیمی و محیطی سطح زمین محسوب می شود. همچنین از پارامترهای اساسی در خصوصیات فیزیک سطح زمین در همه مقیاس ها از محلی تا جهانی است. در حال حاضر مهم ترین منبع داده های اقلیمی ایستگاه های هواشناسی می باشند و این ایستگاه ها آمار اقلیمی نقاط خاصی را ارائه می دهند در حالی که دما ممکن است در فواصل مختلف از این ایستگاه ها متحرک بوده و نسبت به ایستگاه مورد نظر کاهش یا افزایش داشته باشد. از این رو نیاز به تکنولوژی ای که بتواند کاستی های ایستگاه های هواشناسی را در محاسبه دما در فواصل نمونه برداری و در مکان های صعب العبور که امکان احداث ایستگاه هواشناسی وجود ندارد برطرف کند ضروری است. در سال های اخیر علوم جدیدی مانند سنجش از دور روش های جدیدی را برای نظارت بر محیط و کسب، ارزیابی و تجزیه و تحلیل داده های محیطی فراهم آورده است و قابلیت ارائه طیف وسیعی از پارمترهای مربوط به محیط را دارا می باشد.این تکنولوژی به عنوان یک منبع مهم و فزاینده از اطلاعات برای مطالعه تغییرات اقلیمی که بر میزان دمای سطح زمین تأثیر مستقیم دارد مطرح می شود. در طی دو دهه گذشته برای محاسبه دمای سطح زمین 18 الگوریتم توسعه داده شده است که این الگوریتم ها در چهار دسته؛ مدل های وابسته به گسیلمندی، مدل های دو فاکتوره، مدل های پیچیده و مدل های بر مبنای رادیانس قرار دارند. بررسی نتایج مقایسه های انجام گرفته بین الگوریتم های مختلف نشان می دهد که الگوریتم های مختلف عملکرد متفاوتی را در موقعیت های مختلف با آب و هوای متفاوت جغرافیایی دارند. هدف از این تحقیق مقایسه انواع الگوریتم های محاسبه LST برای تصاویر سنجنده MODIS و تعیین بهترین الگوریتم برای استان آذربایجان شرقی می باشد.مواد و روش ها برای تبدیل ارزش های رقومی به تابش طیفی برای باندهای حرارتی تصاویر سنجنده MODIS استفاده قرار گرفت.تبدیل تابش طیفی به بازتاب طیفی با استفاده از رابطه پلانک، داده های حرارتی سنجنده MODIS، زمانی که توان تشعشعی آن ها حداکثر یک در نظر گرفته شوند، قابلیت تبدیل از تابش طیفی به بازتاب طیفی رادارند.در برآورد گسیلمندی سطحی از روش آستانه گذاری شاخص تفاضل نرمال شده گیاهی NDVI استفاده شد. جهت مشخص نمودن ویژگی های خاک در هر پیکسل و محاسبه میزان گسیلمندی و اختلاف گسیلمندی، توان تشعشعی به سه دسته تقسیم گردید؛ 0.2>NDVI به عنوان خاک خشک در نظر گرفته شده وتوان تشعشعی برای آن معادل 0.978 لحاظ می گردد. 0.5NDVI نتایج و بحث در بین 18 الگوریتم محاسبه دمای سطح زمین برای تصاویر سنجنده MODIS به ترتیب؛ الگوریتم سوبرینو با مقدار RMSE، 1.79 بیشترین دقت، الگوریتم کول کاسلیس و پراتا با مقدار RMSE، 2.58 در جایگاه دوم و همچنین الگوریتم های سالیسبوری و سوبرینو با مقدار RMSE، 2.79 جایگاه سومی را برای محاسبه LST در بین سایر الگوریتم ها دارا می باشند. الگوریتم کیین با مقدار RMSE، 5.28 کم ترین دقت را برای محاسبه LST به خود اختصاص داده است.نتیجه گیری بررسی اطلاعات بدست آمده از مقایسه الگوریتم های پنجره مجزاء بیانگر تبعیت کلی دماهای محاسبه شده از شرایط توپوگرافی منطقه است، به طوری که تقریباً کمترین مقادیر درجه حرارت در تمام الگوریتم ها مربوط به قسمت های با ارتفاع بیشتر (کوهستانی) و پوشش سبز منطقه است و مقادیر دما در نواحی دارای ارتفاع پایین و فاقد پوشش گیاهی متراکم افزایش یافته است.
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Asadzadeh A, Faith H, Shawl M. 2015. Spatial Inequalities in the Development of the Agricultural Sector of East Azerbaijan Province. Journal of Space Economics and Rural Development, 4(2): 41-45. (In Persion)
Alavi Panah SK. 2016. Thermal Remote Sensing and its Application in Earth Sciences, Third Edition, University of Tehran Press, 666 p. (In Persion)
Bakhtiari B, Delgarm S, Rezazadeh M. 2016. Selecting the most appropriate split-window algorithm for land surface temperature estimation using MODIS sensor (Case study: Kerman plain). Journal of Water and Soil Conservation, 23(2): 81-98. (In Persion)
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Bulivoury RE, Hartford RA, Eidenshink JC. 1993. Using NDVI to assess departure from average greenness and its relation to the fire business. Intermountain Research Station: USDA Forest Service, 8: 121-137.
Becker F, Li Z-L. 1990. Towards a local split window method over land surfaces. Remote Sensing, 11(3): 369-393. doi:https://doi.org/10.1080/01431169008955028.
Cao L, Li P, Zhang L, Chen T. 2008. Remote sensing image-based analysis of the relationship between urban heat island and vegetation fraction. Paper presented at the The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B7. Beijing 2008, 1379-1384.
Carlson TN, Ripley DA. 1997. On the relation between NDVI, fractional vegetation cover, and leaf area index. Remote Sensing of Environment, 62(3): 241-252. doi:https://doi.org/10.1016/S0034-4257(97)00104-1.
Chehbouni A, Lo Seen D, Njoku EG, Monteny BM. 1996. Examination of the difference between radiative and aerodynamic surface temperatures over sparsely vegetated surfaces. Remote Sensing of Environment, 58(2): 177-186. doi:https://doi.org/10.1016/S0034-4257(96)00037-5.
Cole A, Menenti M, Feddes R, Holtslag A. 1994. A remote sensing surface energy balance algorithm for land (SEBAL) 1 Formulation. Journal of Hydrology, 212(3): 198-212.
Coll C, Caselles V, Sobrino JA, Valor E. 1994. On the atmospheric dependence of the split-window equation for land surface temperature. Remote Sensing, 15(1): 105-122. doi:https://doi.org/10.1080/01431169408954054.
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Eskandari S. 2019. Comparison of different algorithms for preparing land cover map in sensitive habitats of Zagros using Sentinel 2 satellite image (Case study: part of Ilam province). Journal of RS and GIS for Natural Resources, 10(1): 72-87. (In Persion)
Emami H, Mojarradi B, Safari A. 2016. Presenting a method for assessing the accuracy and validation of land surface temperature from remote sensing data: a case study of Fars province. Journal of Mapping Science and Technology, 6(1): 1-17. (In Persion)
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Faizizadeh B, Dideban Kh, Gholamnia Kh. 2016. Estimation of land surface temperature using Landsat 8 satellite images and a split-window algorithm (Case study: Mahabad basin). Journal of Sepehr, 25(98): 171-181. (In Persion)
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