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A generic framework for modeling diurnal land surface temperatures with remotely sensed thermal observations under clear sky

机译:在晴朗的天空下利用遥感的热观测来模拟昼夜地表温度的通用框架

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The modeling of diurnal land surface temperature (LST) is crucial to extend the temporally discrete satellite thermal observations in application to detect the surface property (such as thermal inertia) and fluxes (such as soil heat flux and evapotranspiration) that are important to climate change studies. This paper proposed a generic framework (GEM) for modeling the LST dynamics in clear-sky periods. This was performed by modeling the ground-surface heat flux, which was then transformed into temperature using the surface energy balance and heat conduction equation. Three terms of fluxes were incorporated into GEM, including the nonhomogeneous term depicting the approximate upward flux, the harmonic term representing the approximate solar radiation, and the residue term involving the surplus atmosphere-related flux variations. In a single diurnal temperature cycle (DTC), we derived seven cases of the GEM, i.e., from the GEM-I to -VII, in which two to twelve controlling parameters are required. These controlling parameters are taken as unknowns in backward inversion using temporally discrete surface temperatures. Validations were performed using in-situ brightness temperatures, and Moderate Resolution Imaging Spectroradiometer (MODIS) and Spinning Enhanced Visible and Infrared Imager (SEVIRI) LSTs. The results show that the accuracy generally increases from GEM-I to -VII, with the mean absolute error decreasing from 1.71 to 0.33 degrees C. Particularly, GEM-II and -III can be used to normalize the four MODIS LSTs in a DTC without additional information required; and GEM-VI and -VII are useful once high accuracy is required. Further modeling also indicates that GEM is capable of interpolating LSTs under nonstandard cases with arbitrary starting time, duration length, and local latitude. We consider this study could provide practitioners more options within particular applications for modeling the temperature dynamics under diverse requirements of modeling accuracy and controlling parameter number. (C) 2014 Elsevier Inc. All rights reserved.
机译:昼夜地表温度(LST)的建模对于扩展时间离散卫星热观测的应用至关重要,该观测在应用中对气候变化至关重要的地表特性(例如热惯性)和通量(例如土壤热通量和蒸散量)学习。本文提出了一个通用框架(GEM),用于在晴天期间为LST动力学建模。这是通过对地表热通量进行建模来实现的,然后使用表面能平衡和热传导方程将其转换为温度。 GEM中包含了三项通量,其中包括描述近似向上通量的非均匀项,代表近似太阳辐射的谐波项以及涉及与大气有关的通量变化过多的残差项。在单个昼夜温度周期(DTC)中,我们从GEM-1至-VII导出了7个GEM实例,其中需要2至12个控制参数。这些控制参数在使用时间离散表面温度的反向反演中被视为未知数。使用原位亮度温度,中分辨率成像光谱仪(MODIS)和旋转增强型可见光和红外成像仪(SEVIRI)LST进行验证。结果表明,精度通常从GEM-1提高到-VII,平均绝对误差从1.71降低到0.33摄氏度。特别是,GEM-II和-III可用于归一化DTC中的四个MODIS LST,而无需所需的其他信息;一旦需要高精度,GEM-VI和-VII就很有用。进一步的建模还表明,GEM能够在非标准情况下以任意开始时间,持续时间长度和本地纬度对LST进行插值。我们认为这项研究可以为从业人员在特定应用中提供更多选择,以在建模精度和控制参数数量的各种要求下对温度动态建模。 (C)2014 Elsevier Inc.保留所有权利。

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