Recovering land surface temperature under cloudy skies for potentially deriving surface emitted longwave radiation by fusing MODIS and AMSR-E measurements

Tianxing Wang, Jiancheng Shi, G. Yan, T. Zhao, Dabin Ji, C. Xiong
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引用次数: 10

Abstract

Longwave radiation is a key component of total energy that drives surface energy balance at the interface between the surface and atmosphere. To date, a number of algorithms have been developed toward accurately estimating surface longwave radiation from remotely sensed data. While most of these existing algorithms can only derive longwave radiation under clear-sky conditions due to the limited penetration of optical remote sensing thus leading to spatial incontinuity in derived radiation map. Wherein the land surface temperature (LST) play a key role in longwave radiation estimation, especially for surface emitted (upwelling) and net longwave flux. If LSTs under cloudy area can be recovered, the derivation of surface longwave ration under cloudy conditions would be straightforward. To this end, in this paper, a fusing strategy is proposed to combine the LST measurements from MODIS and AMSR-E. The results show that the proposed fusing strategy for combining microwave and optical space-based measurements in recovering surface LST under cloudy conditions is very effective. By fusion, the spatial coverage of valid LSTs over the globe is highly improved.
通过融合MODIS和AMSR-E测量数据,恢复多云天气下地表温度,从而可能得到地表发射的长波辐射
长波辐射是总能量的一个关键组成部分,它驱动地表与大气交界面的地表能量平衡。迄今为止,已经开发了许多算法来精确估计地表长波辐射的遥感数据。但由于光学遥感的穿透能力有限,现有算法大多只能在晴空条件下导出长波辐射,导致导出的辐射图存在空间不连续性。其中地表温度(LST)在长波辐射估算中起着关键作用,特别是地表发射(上升流)和净长波通量。如果能恢复多云地区的地表长波比,那么多云条件下地表长波比的推导就很简单了。为此,本文提出了一种融合MODIS和AMSR-E测量数据的LST融合策略。结果表明,提出的微波与光学天基测量相结合的融合策略在阴天条件下恢复地表温度是非常有效的。通过融合,有效地表温度在全球范围内的空间覆盖得到了很大的提高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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