A new feedback on climate change from the hydrological cycle
Williams, Paul D.; Guilyardi, Eric; Sutton, Rowan; Gregory, Jonathan; Madec, Gurvan. 2007 A new feedback on climate change from the hydrological cycle. Geophysical Research Letters, 34. L08706. 10.1029/2007GL029275
Full text not available from this repository.Abstract/Summary
An intensification of the hydrological cycle is a likely consequence of global warming. But changes in the hydrological cycle could affect sea-surface temperature by modifying diffusive ocean heat transports. We investigate this mechanism by studying a coupled general circulation model sensitivity experiment in which the hydrological cycle is artificially amplified. We find that the amplified hydrological cycle depresses sea-surface temperature by enhancing ocean heat uptake in low latitudes. We estimate that a 10% increase in the hydrological cycle will contribute a basin-scale sea-surface temperature decrease of around 0.1°C away from high latitudes, with larger decreases locally. We conclude that an intensified hydrological cycle is likely to contribute a weak negative feedback to anthropogenic climate change.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1029/2007GL029275 |
ISSN: | 0094-8276 |
Additional Keywords: | climate feedbacks; hydrological cycle; salinity |
Date made live: | 10 Dec 2008 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/164342 |
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