Impacts of climate change on air-sea exchanges of heat and water
Impacts of climate change on air-sea exchanges of heat and water
Changes in the air-sea fluxes of heat and freshwater are expected as a result of anthropogenic climate change. Studies of increasing observed ocean heat content place a limit of about 0.5 W m-2 on the increase in the global ocean mean net surface heat flux. Given the high level of uncertainty in available flux datasets this signal is likely to be very difficult to detect. A similar situation holds for the surface freshwater flux, for which there are additional problems associated with obtaining reliable long-term estimates of precipitation. Observations of changing ocean salinity suggest a strengthening of the hydrological cycle but further research is required to link this to changing freshwater flux. Variations in freshwater exchanges in the UK marine environment may also occur as a result of shifts in the spatial patterns of the major modes of atmospheric variability.
89-90
Josey, S.
2252ab7f-5cd2-49fd-a951-aece44553d93
Berry, D.I.
55ffc590-f459-49c8-aecf-842d65aeb0fb
Marine Climate Change Impacts Partnership, Lowestoft, UK.
2013
Josey, S.
2252ab7f-5cd2-49fd-a951-aece44553d93
Berry, D.I.
55ffc590-f459-49c8-aecf-842d65aeb0fb
Josey, S. and Berry, D.I.
,
Marine Climate Change Impacts Partnership, Lowestoft, UK.
(2013)
Impacts of climate change on air-sea exchanges of heat and water.
In,
Buckley, P.J., Baxter, J.M. and Wallace, C.J.
(eds.)
Marine Climate Change Impacts Partnership Science Review 2013.
Lowestoft, UK.
MCCIP, .
Record type:
Book Section
Abstract
Changes in the air-sea fluxes of heat and freshwater are expected as a result of anthropogenic climate change. Studies of increasing observed ocean heat content place a limit of about 0.5 W m-2 on the increase in the global ocean mean net surface heat flux. Given the high level of uncertainty in available flux datasets this signal is likely to be very difficult to detect. A similar situation holds for the surface freshwater flux, for which there are additional problems associated with obtaining reliable long-term estimates of precipitation. Observations of changing ocean salinity suggest a strengthening of the hydrological cycle but further research is required to link this to changing freshwater flux. Variations in freshwater exchanges in the UK marine environment may also occur as a result of shifts in the spatial patterns of the major modes of atmospheric variability.
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Published date: 2013
Organisations:
Marine Systems Modelling, Marine Physics and Ocean Climate
Identifiers
Local EPrints ID: 362462
URI: http://eprints.soton.ac.uk/id/eprint/362462
PURE UUID: 15dadbbd-fe77-4454-87a9-8a65120e2168
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Date deposited: 24 Feb 2014 17:14
Last modified: 09 Apr 2024 09:44
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Contributors
Author:
S. Josey
Author:
D.I. Berry
Editor:
P.J. Buckley
Editor:
J.M. Baxter
Editor:
C.J. Wallace
Corporate Author: Marine Climate Change Impacts Partnership, Lowestoft, UK.
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