Impact of Soil Moisture Dynamics on ASAR σ(o) Signatures and Its Spatial Variability Observed over the Tibetan Plateau

This paper reports on the analysis of a 2.5 year-long time series of ASAR wide swath mode (WSM) observations for characterizing the soil moisture dynamics. The employed ASAR WSM data set consists of 152 VV-polarized scenes acquired in the period between April 2005 and September 2007 over the Naqu river basin located on the Tibetan Plateau. For four different spatial domains, with areas of 30×30 km(2), 5×5 km(2) and (two domains of) 1×1 km(2), the mean backscatter (σ(o)) and the standard deviation (stdev) have been computed for each ASAR acquisition. Comparison of the mean σ(o) values with the stdev values results in a specific triangular distribution of data points for all spatial domains. Analysis of the mean σ(o) and stdev with respect to in-situ soil moisture measurements demonstrates that this triangular shaped distribution can be explained by soil moisture dynamics during monsoon and winter periods. This shows that the relationship between the spatial mean soil moisture and variability is not uniquely defined and may change throughout seasons. Downscaling of coarse resolution soil moisture products should, therefore, be ideally based on additional near real time data sources. In this context, the presented results could form a basis for the development of SAR-based soil moisture downscaling methodologies.