Using area-average remotely sensed surface soil moisture in multipatch land data assimilation systems

In coming years, Land Data Assimilation Systems (LDAS) two-dimensional (2-D ) arrays of the relevant land-surface model) are likely to become the routi ne mechanism by which many predictive weather and climate models will be in itiated. If this is so, it will be via assimilation into the LDAS that othe r data relevant to the land surface, such as remotely sensed estimates of s oil moisture, will find value. This paper explores the potential for using low-resolution, remotely sensed observations of microwave brightness temper ature to infer soil moisture in an LDAS with a "mosaic-patch" representatio n of land-surface heterogeneity, by coupling the land-surface model in the LDAS to a physically realistic microwave emission model. The past descripti on of soil water movement by the LDAS is proposed as the most appropriate, LDAS-consistent basis for using remotely sensed estimates of surface soil m oisture to infer soil moisture at depth, and the plausibility of this propo sal is investigated. Three alternative methods are explored for partitionin g soil moisture between modeled patches while altering the area-average soi l moisture to correspond to the observed, pixel-average microwave brightnes s temperature, namely, 1) altering the soil moisture by a factor, which is the same for all the patches in the pixel, 2) altering the soil moisture by adding an amount that is the same for all the patches in the pixel, and 3) altering the change in soil moisture since the last assimilation cycle by a factor which is the same for all the patches in the pixel. In each case, an iterative procedure is required to make the adjustment. Comparison is ma de between these alternative procedures for a hypothetical pixel that conta ins eight individual patches (three different vegetation types growing both in clay and sand, plus one patch of bare soil and one of open water) using a mosaic-patch version of the MICRO-SWEAT model. When the applied forcing variables are artificially degraded, all three methods provide similar, imp roved descriptions of the time-evolution of soil moisture in the pixel as a whole and of the deep soil moisture for each patch. However, in each case, the ability of the LDAS to correctly describe the separate evolution of su rface soil moisture in each patch is imperfect.