Abstract

Previous validation studies have demonstrated the accuracy of the Metop-A ASCAT soil moisture (SM) product, although over- and underestimation during different seasons of the year suggest a need for improving the retrieval algorithm. In this study, we analyzed whether adapting the vegetation characterization based on global parameters to regional conditions improves the seasonal representation of SM and vegetation optical depth ( τ ). SM and τ are retrieved from ASCAT using both a seasonal (mean climatological) and a dynamic vegetation characterization that allows for year-to-year changes. The retrieved SM and τ are compared with in situ and satellite SM, and with vegetation products (SMAP, AMSR2, and SPOT-VGT/PROBA-V). The study region is set in an agricultural area of Lower Austria that is characterized by heterogeneous land cover and topography, and features an experimental catchment equipped with a SM network (HOAL SoilNet). We found that a stronger vegetation correction within the SM retrieval improves the SM product considerably (increase of the Spearman correlation coefficient r s by 0.15 on average, and r s comparable to SMAP and AMSR2). The vegetation product derived with a dynamic vegetation characterization compares well to the reference datasets and reflects vegetation dynamics such as start and peak of season and harvest. Although some vegetation effects cannot be corrected by the adapted vegetation characterization, our results demonstrate the benefits of a parameterization optimized for regional conditions in this temperate climate zone.

Highlights

  • Soil moisture (SM) plays an important role in the water and carbon cycle and needs to be considered in a number of related applications

  • We analyzed the retrieval of surface soil moisture (SM) and vegetation optical depth τ from Metop-A Advanced Scatterometer (ASCAT) over a region in Lower Austria

  • Both SM and τ have been retrieved from ASCAT backscatter values using a seasonal and a dynamic vegetation characterization, which takes into account year-to-year changes

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Summary

Introduction

Soil moisture (SM) plays an important role in the water and carbon cycle and needs to be considered in a number of related applications. The Soil Moisture Ocean Salinity (SMOS) [14] and Soil Moisture Active Passive (SMAP) [15] missions are dedicated SM missions operating in L-band, providing global passive SM observations. Another sensor that can be used for the retrieval of global SM, though not designed for this purpose, is the Advanced Microwave Scanning Radiometer 2 (AMSR2), a passive multi-frequency instrument on board GCOM-W1 [16]. An active C-band sensor suitable for SM retrieval is the Advanced Scatterometer (ASCAT) on board the Metop satellites

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