Fig. 5: Partitioning the model ensemble into deep and shallow soil ESMs. | npj Climate and Atmospheric Science

Fig. 5: Partitioning the model ensemble into deep and shallow soil ESMs.

From: Observations indicate regionally misleading wetting and drying trends in CMIP6

Fig. 5: Partitioning the model ensemble into deep and shallow soil ESMs.

Above: Rescaled weighted mTWS MMMed trend (1950–2100) for models with a total thickness of all soil layers of a >4.6 m (deep soil; 8 models), and b ≤4.6 m (shallow soil; 9 models). Below: Regions of high model consensus regarding the direction of mTWS trends, distinguished into high/low temporal consensus and fit/no fit to GRACE/DA TWS trends for c deep soil models, and d shallow soil models.

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