A novel approach combining satellite and in situ observations to estimate the daytime variation of land surface temperatures for all sky conditions

IF 5.7 Q1 ENVIRONMENTAL SCIENCES
Anand K. Inamdar, Ronald D. Leeper
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引用次数: 0

Abstract

Land surface temperature (LST) and its diurnal variability are key to understanding the land-atmosphere interactions, hydrological processes and climate change. However, at any given point in time approximately half of the Earth's surface is covered by clouds. This restricts the availability of LST through satellite remote sensing, which works best under clear skies. However, in situ observations continue to monitor atmospheric conditions beneath the clouds that could complement satellite measurements during cloudy conditions. The present study explores a novel approach to estimate hourly LST during the daylight hours using remotely sensed surface solar absorption and in situ observations of daily LST extremes (maximum and minimum) together with an adaptive non-linear fitting approach. A learning algorithm trained against in-situ measurements of LST extrema and diurnal cycle of surface solar absorption together with the associated linear correlation between the two parameters, is used to estimate an optimized set of parameters to approximate hourly LST for each day during the daylight hours between sunrise and sunset. Results show that the method captures the intra-day variability of LST very well under most sky conditions with rms errors below 1.5 K.

结合卫星和现场观测估算所有天空条件下陆地表面温度日间变化的新方法
陆地表面温度(LST)及其昼夜变化是了解陆地-大气相互作用、水文过程和气候变化的关键。然而,在任何特定时间点,地球表面约有一半被云层覆盖。这就限制了通过卫星遥感获得 LST 的可能性,因为卫星遥感在晴朗的天空下效果最佳。不过,现场观测可以继续监测云层下的大气条件,从而在多云条件下对卫星测量结果进行补充。本研究探索了一种新方法,利用遥感地表太阳吸收率和原地观测到的每日 LST 极端值(最大值和最小值)以及自适应非线性拟合方法来估算白天的每小时 LST。根据对 LST 极值和地表太阳吸收率昼夜周期的现场测量结果以及这两个参数之间的相关线性关系训练的学习算法,用于估算一组优化参数,以近似计算日出和日落之间每天白天的每小时 LST。结果表明,该方法在大多数天空条件下都能很好地捕捉到 LST 的日内变化,均方根误差低于 1.5 K。
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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来源期刊
CiteScore
12.20
自引率
0.00%
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