Global water cycle amplifying at less than the Clausius-Clapeyron rate

Skliris, Nikolaos; Zika, Jan D.; Nurser, George; Josey, Simon A. ORCID: https://orcid.org/0000-0002-1683-8831; Marsh, Robert. 2016 Global water cycle amplifying at less than the Clausius-Clapeyron rate. Scientific Reports, 6. 38752. 10.1038/srep38752

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Official URL: http://dx.doi.org/10.1038/srep38752

Abstract/Summary

A change in the cycle of water from dry to wet regions of the globe would have far reaching impact on humanity. As air warms, its capacity to hold water increases at the Clausius-Clapeyron rate (CC, approximately 7% °C−1). Surface ocean salinity observations have suggested the water cycle has amplified at close to CC following recent global warming, a result that was found to be at odds with state-of the art climate models. Here we employ a method based on water mass transformation theory for inferring changes in the water cycle from changes in three-dimensional salinity. Using full depth salinity observations we infer a water cycle amplification of 3.0 ± 1.6% °C−1 over 1950–2010. Climate models agree with observations in terms of a water cycle amplification (4.3 ± 2.0% °C−1) substantially less than CC adding confidence to projections of total water cycle change under greenhouse gas emission scenarios.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1038/srep38752
ISSN:	2045-2322
Date made live:	13 Dec 2016 13:28 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/515478

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1038/srep38752

ISSN:

2045-2322

Date made live:

13 Dec 2016 13:28 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/515478