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Potential of Sentinel-1 Surface Soil Moisture Product for Detecting Heavy Rainfall in the South of France

机译:Sentinel-1表面土壤水分产品在法国南部检测暴雨的潜力

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摘要

The objective of this paper is to present an analysis of Sentinel-1 derived surface soil moisture maps (S1-SSM) produced with high spatial resolution (at plot scale) and a revisit time of six days for the Occitanie region located in the South of France as a function of precipitation data, in order to investigate the potential of S1-SSM maps for detecting heavy rainfalls. First, the correlation between S1-SSM maps and rainfall maps provided by the Global Precipitation Mission (GPM) was investigated. Then, we analyzed the effect of the S1-SSM temporal resolution on detecting heavy rainfall events and the impact of these events on S1-SSM values as a function of the number of days that separated the heavy rainfall and the S1 acquisition date (cumulative rainfall more than 60 mm in 24 hours or 80 mm in 48 hours). The results showed that the six-day temporal resolution of the S1-SSM map doesn’t always permit the detection of an extreme rainfall event, because confusion will appear between high S1-SSM values due to extreme rainfall events occurring six days before the acquisition of S1-SSM, and high S1-SSM values due to light rain a few hours before the acquisition of Sentinel-1 images. Moreover, the monitoring of extreme rain events using only soil moisture maps remains difficult, since many environmental parameters could affect the value of SSM, and synthetic aperture radar (SAR) doesn’t allow the estimation of very high soil moistures (higher than 35 vol.%).
机译:本文的目的是分析Sentinel-1衍生的地表土壤水分图(S1-SSM),该图以较高的空间分辨率(按地块比例)生成,并且位于南部的Occitanie地区的重访时间为6天。法国是降水数据的函数,目的是研究S1-SSM图在探测强降雨方面的潜力。首先,研究了全球降水任务(GPM)提供的S1-SSM图和降雨图之间的相关性。然后,我们分析了S1-SSM时间分辨率对检测暴雨事件的影响以及这些事件对S1-SSM值的影响,这些事件是将暴雨和S1采集日期(累积降雨)分开的天数的函数在24小时内超过60毫米或在48小时内超过80毫米)。结果表明,S1-SSM图的六天时间分辨率并不总是能够检测到极端降雨事件,因为在采集前六天发生了极端降雨事件,因此在高S1-SSM值之间会出现混淆采集Sentinel-1图像前几个小时,由于小雨造成的S1-SSM值较高,并且S1-SSM值较高。此外,由于许多环境参数可能会影响SSM的值,并且仅使用合成孔径雷达(SAR)不能估算非常高的土壤湿度(高于35 vol 。%)。

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