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On the sources of global land surface hydrologic predictability

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Fig. 1. lead-1, -3 and -6 months for forecast initialization on Spatial variability of κ (ratio of the standard deviation of initial total moisture to total precipitation during the forecast period) at (a) 1 January, (b) 1 April, (c) 1 July and (d) 1 October.
Fig. 2. Fig. 2: RMSE ratio for soil moisture (SM) forecasts at lead-1, -3 and -6 months for  RMSE ratio for soil moisture (SM) forecasts at lead-1, -3 and -6 months for forecast initialization on (a) 1 January, (b) 1 April,(c) 1 July and (d) 1 October.
Table 1. K¨oppen–Geiger Climate Classification (source: Kottek et al., 2006).
Fig. 4.tio (RMSE/RMSE) at lead-1, -3 and -6 months for SMFig. 4: Pattern correlation between Kappa and inverse RMSE ratio (RMSE Pattern correlation between kappa and inverse RMSE ra-Rev-ESPESPforecasts initialized on 1 January, 1 April, 1 July and 1 October.Rev-ESP/
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