来自智利阿瓜斯卡连特斯盐湖的雷达和多光谱遥感上的情景事件

A. Delsouc, M. Barber, W. Pérez-Martínez, I. Briceño-De-Urbaneja
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引用次数: 0

摘要

有限的幕式变化发生在短时间和大空间范围内。极端天气条件通常会引起有限的间歇性变化。Sentinel-1在高原冬季(2015年3月和2017年6月)、2018年南方冬季和2017-2018年春季获取了智利阿瓜斯卡兰特斯盐湖的雷达图像,展示了远程监测情景事件的能力。后向散射功率的结果是令人鼓舞的,并且在c波段显示出VV极化的阶段性变化。无论是高原冬季还是南方冬季,阿瓜斯卡兰特斯盐湖的地表特征都随着降雪的变化而变化,在盐盘地壳上有干雪存在时,后向散射增加。2017-2018年春季与融雪相关的洪水事件显示,池塘水面上的后向散射信号减少,当风吹过水面时,后向散射信号增加。对盐湖的遥感观测可以提供一种监测盐湖表面变化的手段,并更好地了解相关的气候偶发事件过程。此外,它还有助于更好地了解干旱地区的环境变化和全球气候变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Episodic Events On Radar And Multispectral Remote Sensors From Salar De Aguas Calientes, Chile
Restricted episodic changes occurred in a short time period and over large spatial extents. Extreme weather conditions usually give rise to restricted episodic changes. Sentinel-1 radar images of the Salar de Aguas Calientes in Chile acquired in the Altiplanic winter (March 2015 and June 2017), 2018 austral winter and 2017-2018 springtime, demonstrates the ability to monitor episodic events remotely. The results of the backscattered power are encouraging and show episodic variations in VV polarization at C-band. The surface features in Salar de Aguas Calientes Sur change in response to snowfalls during either the Altiplanic or austral winter with an increase of the backscattering in presence of dry snow over the salt pan crust. Flooding events related to snow-melting during spring 2017-2018 showed a decrease in the backscattering signal over ponded water and an increase when wind blows over the water. Remote-sensing observations of the salar can provide a means for monitoring changes in the surface of the salar and a better understanding of the associated climatic episodic event processes. Furthermore, it can help to have a better understanding of environmental changes in arid regions and the understanding of global climate change.
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