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For the development of alert systems for soil slip occurrence, it is important to evaluate the degree of saturation of shallow soils (S r ) over wide areas. Taking into account the possibility to estimate spatial and temporal variation of soil moisture using remote sensing techniques, a possible correlation between S r and the daily output of a sequential data assimilation system called ACHAB (Assimilation Code for HeAt and moisture Balance) has been studied. ACHAB is based on integrated use ofdoi:10.4236/ijg.2010.12008 fatcat:5iji5fkzdfaa3hzh26rz34ok2u