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  • Gridded daily precipitation obtained by merging soil moisture-derived and passive microwave rainfall estimatesobtained through the application of SM2RAIN to the SSMASCAT-A/B-NRT-O12.5 (H16and H101) soil moisture products, with the H-AUX-23 rainfall estimates.

  • Percent of saturated soil moisture, 25km resolution

  • The EDO Soil Moisture Anomaly (SMA) indicator is computed every 10-day as anomalies of soil moisture index derived from the JRC’s in-house LISFLOOD hydrological model.

  • Soil moisture derived from passive microwave at 1km resolution, downscaled to 100m using Sentinel-2

  • Soil moisture derived from the Backus-Gilbert interpolated radiometer brightness temperature measurements, posted at 9 km.

  • Soil moisture content in the surface layer (0.5-2 cm) express in degree of saturation (0 – 100 %) generated from ASCAT Metop-B at 12.5 km sampling, processed shortly after each satellite orbit completion.