A new feedback on climate change from the hydrological cycle
A new feedback on climate change from the hydrological cycle
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.
climate feedbacks, hydrological cycle, salinity
L08706
Williams, Paul D.
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Guilyardi, Eric
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Sutton, Rowan
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Gregory, Jonathan
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Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864
2007
Williams, Paul D.
6f9d4400-93e5-4c43-8ad1-630c0c474c3b
Guilyardi, Eric
7a596a3f-7c16-4d5b-8fa8-13848959694d
Sutton, Rowan
6ec4d816-4095-4d4b-a661-3a6f26d580be
Gregory, Jonathan
b5f3c77e-aefb-495e-959d-ae060e415257
Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864
Williams, Paul D., Guilyardi, Eric, Sutton, Rowan, Gregory, Jonathan and Madec, Gurvan
(2007)
A new feedback on climate change from the hydrological cycle.
Geophysical Research Letters, 34, .
(doi:10.1029/2007GL029275).
Abstract
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.
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Published date: 2007
Keywords:
climate feedbacks, hydrological cycle, salinity
Organisations:
National Oceanography Centre,Southampton
Identifiers
Local EPrints ID: 64342
URI: http://eprints.soton.ac.uk/id/eprint/64342
ISSN: 0094-8276
PURE UUID: 7029d07a-954f-4a0b-8a40-2655170b7122
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Date deposited: 10 Dec 2008
Last modified: 15 Mar 2024 11:48
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Contributors
Author:
Paul D. Williams
Author:
Eric Guilyardi
Author:
Rowan Sutton
Author:
Jonathan Gregory
Author:
Gurvan Madec
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