Soil moisture from operational meteorological satellites

被引:0
作者
Wolfgang Wagner
Vahid Naeimi
Klaus Scipal
Richard de Jeu
José Martínez-Fernández
机构
[1] Vienna University of Technology,Institute of Photogrammetry and Remote Sensing
[2] European Centre for Medium-Range Weather Forecasts (ECMWF),Department of Hydrology and GeoEnvironmental Sciences
[3] Vrije Universiteit Amsterdam,Department of Geography
[4] University of Salamanca,undefined
来源
Hydrogeology Journal | 2007年 / 15卷
关键词
Remote sensing; Soil moisture; Unsaturated zone; Scale effects; Satellites;
D O I
暂无
中图分类号
学科分类号
摘要
In recent years, unforeseen advances in monitoring soil moisture from operational satellite platforms have been made, mainly due to improved geophysical retrieval methods. In this study, four recently published soil-moisture datasets are compared with in-situ observations from the REMEDHUS monitoring network located in the semi-arid part of the Duero basin in Spain. The remotely sensed soil-moisture products are retrieved from (1) the Advanced Microwave Scanning Radiometer (AMSR-E), which is a passive microwave sensor on-board NASA’s Aqua satellite, (2) European Remote Sensing satellite (ERS) scatterometer, which is an active microwave sensor on-board the two ERS satellites and (3) visible and thermal images from the METEOSAT satellite. Statistical analysis indicates that three satellite datasets contribute effectively to the monitoring of trends in surface soil-moisture conditions, but not to the estimation of absolute soil-moisture values. These sensors, or rather their successors, will be flown on operational meteorological satellites in the near future. With further improvements in processing techniques, operational meteorological satellites will increasingly deliver high-quality soil-moisture data. This may be of particular interest for hydrogeological studies that investigate long-term processes such as groundwater recharge.
引用
收藏
页码:121 / 131
页数:10
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