Abstract
AbstractUsing a decade of ground‐based soil moisture observations acquired from the United States Department of Agriculture's Soil Climate Analysis Network (SCAN), we calculate the mutual information (MI) content between multiple soil moisture variables and near‐future vegetation condition to examine the existence of emergent drought information in vertically integrated (surface to 60 cm) soil moisture observations (θ0–60 [cm]) not present in either superficial soil moisture observations (θ5 [cm]) or a simple low‐pass transformation of θ5. Results suggest that while θ0–60 is indeed more valuable than θ5 for predicting near‐future vegetation anomalies, the enhanced information content in θ0–60 soil moisture can be effectively duplicated by the low‐pass transformation of θ5. This implies that, for drought monitoring applications, the shallow vertical penetration depth of microwave‐based θ5 retrievals does not represent as large a practical limitation as commonly perceived.
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