Congo Basin Hydrology, Climate, and Biogeochemistry. Группа авторов

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Congo Basin Hydrology, Climate, and Biogeochemistry - Группа авторов


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the observed data were thereafter used for forward prediction based on the hold‐out method of cross‐validation (e.g., Haley, 2017). The stratified partitioning of the data using this approach ensures that each partition includes similar amount of observations from each group. The predicted and observed discharge were then compared using Pearson correlation.

      5.3.1. Characteristics of Extreme Events in the Congo Basin

Schematic illustration of spatiotemporal SPEI patterns of the Congo basin using 12-month gridded SPEI values (a–f). Schematic illustration of estimated areas affected by various drought intensities (extreme, severe, and moderate) over the Congo basin during 1980–2000 (a) and 2001–2015 (b) periods.

      5.3.2. Surface Water Hydrology of the Congo Basin

       Spatial and Temporal Patterns of Land Water Storage


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