Predictable climate impacts of the decadal changes in the ocean in the 1990s

During the 1990s there was a major change in the state of the world's oceans. In particular, the North Atlantic underwent a rapid warming, with sea surface temperatures (SSTs) in the subpolar gyre region increasing by 1°C in just a few years. Associated with the changes in SST patterns were cha...

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Published in:Journal of Climate
Main Authors: Robson, Jon, Sutton, Rowan, Smith, Doug
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2013
Subjects:
Online Access:https://centaur.reading.ac.uk/33649/
https://centaur.reading.ac.uk/33649/1/JCLI-D-12-00827.pdf
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spelling ftunivreading:oai:centaur.reading.ac.uk:33649 2024-09-15T18:22:32+00:00 Predictable climate impacts of the decadal changes in the ocean in the 1990s Robson, Jon Sutton, Rowan Smith, Doug 2013-09-01 text https://centaur.reading.ac.uk/33649/ https://centaur.reading.ac.uk/33649/1/JCLI-D-12-00827.pdf en eng American Meteorological Society https://centaur.reading.ac.uk/33649/1/JCLI-D-12-00827.pdf Robson, J. <https://centaur.reading.ac.uk/view/creators/90002607.html> orcid:0000-0002-3467-018X , Sutton, R. <https://centaur.reading.ac.uk/view/creators/90000057.html> orcid:0000-0001-8345-8583 and Smith, D. (2013) Predictable climate impacts of the decadal changes in the ocean in the 1990s. Journal of Climate, 26 (17). pp. 6329-6339. ISSN 1520-0442 doi: https://doi.org/10.1175/JCLI-D-12-00827.1 <https://doi.org/10.1175/JCLI-D-12-00827.1> Article PeerReviewed 2013 ftunivreading https://doi.org/10.1175/JCLI-D-12-00827.1 2024-06-25T14:55:27Z During the 1990s there was a major change in the state of the world's oceans. In particular, the North Atlantic underwent a rapid warming, with sea surface temperatures (SSTs) in the subpolar gyre region increasing by 1°C in just a few years. Associated with the changes in SST patterns were changes in the surface climate, in particular, a tendency for warm and dry conditions over areas of North America in all seasons, and warm springs and wet summers over areas of Europe. Here, the extent to which a climate prediction system initialized using observations of the ocean state is able to capture the observed changes in seasonal mean surface climate is investigated. Rather than examining predictions of the mid-1990s North Atlantic warming event itself, this study compares hindcasts started before and after the warming, relative to hindcasts that do not assimilate information. It is demonstrated that the hindcasts capture many aspects of the observed changes in seasonal mean surface climate, especially in North, South, and Central America and in Europe. Furthermore, the prediction system retains skill beyond the first year. Finally, it is shown that, in addition to memory of Atlantic SSTs, successfully predicting Pacific SSTs was likely important for the hindcasts to predict surface climate over North America. Article in Journal/Newspaper North Atlantic CentAUR: Central Archive at the University of Reading Journal of Climate 26 17 6329 6339
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collection CentAUR: Central Archive at the University of Reading
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language English
description During the 1990s there was a major change in the state of the world's oceans. In particular, the North Atlantic underwent a rapid warming, with sea surface temperatures (SSTs) in the subpolar gyre region increasing by 1°C in just a few years. Associated with the changes in SST patterns were changes in the surface climate, in particular, a tendency for warm and dry conditions over areas of North America in all seasons, and warm springs and wet summers over areas of Europe. Here, the extent to which a climate prediction system initialized using observations of the ocean state is able to capture the observed changes in seasonal mean surface climate is investigated. Rather than examining predictions of the mid-1990s North Atlantic warming event itself, this study compares hindcasts started before and after the warming, relative to hindcasts that do not assimilate information. It is demonstrated that the hindcasts capture many aspects of the observed changes in seasonal mean surface climate, especially in North, South, and Central America and in Europe. Furthermore, the prediction system retains skill beyond the first year. Finally, it is shown that, in addition to memory of Atlantic SSTs, successfully predicting Pacific SSTs was likely important for the hindcasts to predict surface climate over North America.
format Article in Journal/Newspaper
author Robson, Jon
Sutton, Rowan
Smith, Doug
spellingShingle Robson, Jon
Sutton, Rowan
Smith, Doug
Predictable climate impacts of the decadal changes in the ocean in the 1990s
author_facet Robson, Jon
Sutton, Rowan
Smith, Doug
author_sort Robson, Jon
title Predictable climate impacts of the decadal changes in the ocean in the 1990s
title_short Predictable climate impacts of the decadal changes in the ocean in the 1990s
title_full Predictable climate impacts of the decadal changes in the ocean in the 1990s
title_fullStr Predictable climate impacts of the decadal changes in the ocean in the 1990s
title_full_unstemmed Predictable climate impacts of the decadal changes in the ocean in the 1990s
title_sort predictable climate impacts of the decadal changes in the ocean in the 1990s
publisher American Meteorological Society
publishDate 2013
url https://centaur.reading.ac.uk/33649/
https://centaur.reading.ac.uk/33649/1/JCLI-D-12-00827.pdf
genre North Atlantic
genre_facet North Atlantic
op_relation https://centaur.reading.ac.uk/33649/1/JCLI-D-12-00827.pdf
Robson, J. <https://centaur.reading.ac.uk/view/creators/90002607.html> orcid:0000-0002-3467-018X , Sutton, R. <https://centaur.reading.ac.uk/view/creators/90000057.html> orcid:0000-0001-8345-8583 and Smith, D. (2013) Predictable climate impacts of the decadal changes in the ocean in the 1990s. Journal of Climate, 26 (17). pp. 6329-6339. ISSN 1520-0442 doi: https://doi.org/10.1175/JCLI-D-12-00827.1 <https://doi.org/10.1175/JCLI-D-12-00827.1>
op_doi https://doi.org/10.1175/JCLI-D-12-00827.1
container_title Journal of Climate
container_volume 26
container_issue 17
container_start_page 6329
op_container_end_page 6339
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