Fig. 4: Changes in the normalized streamflow climatology (\({\Delta} (\frac{Q}{P})\)) caused by a +3.0 °C warming. | Communications Earth & Environment

Fig. 4: Changes in the normalized streamflow climatology (\({\Delta} (\frac{Q}{P})\)) caused by a +3.0 °C warming.

From: Interactions between snow cover and evaporation lead to higher sensitivity of streamflow to temperature

Fig. 4

Black dashed lines show binned-average change across different average temperatures (\(\bar T\)) for the selected 214 CAMELS under the “water” scenario, whereas red dashed lines show the changes according to the “snow” scenario. Shaded regions of both curves represent the SD taken from the groups of catchments within the same temperature ranges.

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