Description: |
How the global hydrological cycle responds to surface temperature change has been debated for decades. This debate is crucial to correctly assess the global warming-related climate variability in the water cycle. The authors of this study conclude that precipitation variability on the inter-annual time scale, once the net large-scale dynamic effects particularly associated with ENSO become weak or limited, does not follow surface temperature and related water vapour variations. [Source: International Journal of Climatology]
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