Soil Moisture Active Passive (SMAP) Data for Ground Monitoring during Earthquakes
Publication: Geo-Congress 2023
ABSTRACT
Degree of water saturation in soils has a key role in the response of geotechnical systems to earthquakes. In the absence of a remotely sensed tool to track soil saturation at a global scale, parameters such as annual average of water table depth, historical average of precipitation measurements, and topographic conditions are considered as proxies for soil saturation condition, the Soil Moisture Active Passive (SMAP), an earth observation satellite, has been launched in 2015 by National Aeronautics and Space Administration (NASA) to record soil moisture content in approximately the top 5 cm of the soil layer over the global land area with a three-day average temporal resolution. In addition, assimilating SMAP observations with estimates provided by land surface models, SMAP researchers can monitor root zone soil moisture in the top 1 m of the soil column. This paper shows how SMAP, as a high accuracy and near-real-time database, can be used to study the relationship between soil moisture and seismic ground response, which includes tracking the earth’s surface soil moisture variations caused by seismic events as well as flagging potentially damaged regions for earthquake reconnaissance teams.
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