ارزیابی پارامتر تابش خورشیدی ورودی به زمین حاصل از مدل‌های تجربی و ماهواره‌ای

نوع مقاله : مقاله پژوهشی

نویسندگان

1 استادیار دانشکده مهندسی و فناوری کشاورزی، پردیس کشاورزی و منابع طبیعی دانشگاه تهران

2 دانشجو - دانشکده کشاورزی و منابع طبیعی دانشگاه تهران

3 گروه مهندسی آب دانشگاه گیلان، رشت، گیلان

چکیده

یکی از مهم‌ترین فرآیندهای انتقال آب و انرژی در چرخه هیدرولوژیکی، تبخیر-تعرق است و تابش خورشیدی انرژی لازم برای انجام این فرآیند را تأمین می‌کند. درنتیجه تخمین هرچه دقیق‌تر میزان تبخیر-تعرق به تخمین دقیق میزان تابش خورشیدی وابسته است. این تحقیق با هدف ارزیابی میزان تابش خورشیدی در سطح زمین حاصل از سه روش معادلات تجربی (مدل‌های آنگستروم و هارگریوز-سامانی) مدل‌های فیزیکی داده‌گواری شده (GLDAS/Noah، NCEP/NCAR)و مشاهدات ماهواره‌ای (CM-SAF)با استفاده از اندازه‌گیری‌های زمینی صورت گرفته است. نتایج این تحقیق نشان داد مدل کالیبره شده آنگستروم با ضریب تبیین برابر با 9/0 و SEEبرابر با 58/2 بهترین عملکرد را داشته است. اما دقت این مدل وابسته به روش کالیبراسیون و وجود داده‌های ساعات آفتابی است. محصول تابش سطح زمین مستخرج از GLDAS/Noah با ضریب تبیین و SEEبه ترتیب برابر با 87/0 و 5/3 بهترین کارایی را بعد از مدل واسنجی شده آنگستروم داشت. مدل GLDAS/Noahبا وجود برآورد 2/10 درصدی تابش خورشیدی بیش از اندازه‌گیری زمینی، در مناطقی که کمبود داده هواشناسی وجود دارد می‌تواند کارایی بسیار خوبی داشته باشد.

کلیدواژه‌ها

موضوعات

عنوان مقاله [English]

Evaluation of Incoming Solar Radiation Parameter Derived from Empirical and Satellite Models

نویسندگان [English]

  • Hamideh Noory 1
  • Ali Mokhtari 2
  • Majid Vazifedoust 3
1 Assistance professor, Department of Irrigation and Reclamation Eng., College of Agriculture and Natural Resources, University of Tehran
2 Student of University college of agriculture and natural resources university of Tehran
3 Assistance professor, Water Engineering Department, University of Guilan, Rasht, Iran
چکیده [English]

Evapotranspiration is one of the most important processes in water and radiative transfer in hydrological cycle, and the required energy for this process is provided by solar radiation. Therefore, the accuracy of evapotranspiration estimation is strongly depends on the accuracy of solar radiation estimation. This study was conducted to evaluate the different surface solar radiation models such as empirical models (Angstrom and Hargreaves-Samani), physically-based models (NCEP and GLDAS) and a satellite observation model (CM-SAF). The results showed that the calibrated Angstrom model with R2=0.9 and SEE=2.58 was the most efficient model. However, the accuracy of this model is strongly depends on the calibration procedure and the existence of sunshine data. The GLDAS model with R2= 0.87 and SEE=3.5 was the second most efficient model after calibrated Angstrom model. The GLDAS model, in spite of 10.2% overestimation of surface solar radiation, can be the most efficient model in areas with the lack of meteorological data.

کلیدواژه‌ها [English]

  • Angstrom
  • CM-SAF
  • GLDAS
  • Hargreaves-Samani
  • Surface solar radiation

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تحقیقات آب و خاک ایران
دوره 50، شماره 2
خرداد و تیر 1398
صفحه 353-362

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