Estimations of Land Surface Characteristic Parameters and Turbulent Heat Fluxes over the Tibetan Plateau Based on FY-4A/AGRI Data

被引:0
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作者
Nan Ge
Lei Zhong
Yaoming Ma
Yunfei Fu
Mijun Zou
Meilin Cheng
Xian Wang
Ziyu Huang
机构
[1] University of Science and Technology of China,School of Earth and Space Sciences
[2] CAS Center for Excellence in Comparative Planetology,Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research
[3] Jiangsu Collaborative Innovation Center for Climate Change,College of Earth and Planetary Sciences
[4] Chinese Academy of Science,undefined
[5] CAS Center for Excellence in Tibetan Plateau Earth Sciences,undefined
[6] University of Chinese Academy of Science,undefined
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关键词
FY-4A/AGRI; land surface characteristic parameters; turbulent heat fluxes; Surface Energy Balance System model; Tibetan Plateau; FY-4A/AGRI; 地表特征参数; 湍流热通量; SEBS模型; 青藏高原;
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学科分类号
摘要
Accurate estimates of land surface characteristic parameters and turbulent heat fluxes play an important role in the understanding of land-atmosphere interaction. In this study, Fengyun-4A (FY-4A) Advanced Geostationary Radiation Imager (AGRI) satellite data and the China Land Data Assimilation System (CLDAS) meteorological forcing dataset CLDAS-V2.0 were applied for the retrieval of broadband albedo, land surface temperature (LST), radiation flux components, and turbulent heat fluxes over the Tibetan Plateau (TP). The FY-4A/AGRI and CLDAS-V2.0 data from 12 March 2018 to 30 April 2018 were first used to estimate the hourly turbulent heat fluxes over the TP. The time series data of in-situ measurements from the Tibetan Observation and Research Platform were divided into two halves—one for developing retrieval algorithms for broadband albedo and LST based on FY-4A, and the other for the cross validation. Results show the root-mean-square errors (RMSEs) of the FY-4A retrieved broadband albedo and LST were 0.0309 and 3.85 K, respectively, which verifies the applicability of the retrieval method. The RMSEs of the downwelling/upwelling shortwave radiation flux and downwelling/upwelling longwave radiation flux were 138.87/32.78 W m−2 and 51.55/17.92 W m−2, respectively, and the RMSEs of net radiation flux, sensible heat flux, and latent heat flux were 58.88 W m−2, 82.56 W m−2 and 72.46 W m−2, respectively. The spatial distributions and diurnal variations of LST and turbulent heat fluxes were further analyzed in detail.
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页码:1299 / 1314
页数:15
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