Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters
The trends in marine 10-m wind speed U10 and significant wave height Hs found in two century-long reanalyses are compared against a model-only integration. Reanalyses show spurious trends due to the assimilation of an increasing number of observations over time. The comparisons between model and rea...
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American Meteorological Society
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Online Access: | https://hdl.handle.net/11250/2761403 https://doi.org/10.1175/JCLI-D-19-0540.1 |
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ftunivbergen:oai:bora.uib.no:11250/2761403 2023-05-15T17:33:26+02:00 Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters Meucci, Alberto Young, Ian R. Aarnes, Ole Johan Breivik, Øyvind 2020 application/pdf https://hdl.handle.net/11250/2761403 https://doi.org/10.1175/JCLI-D-19-0540.1 eng eng American Meteorological Society Norges forskningsråd: 256466 EC/H2020/JPI Cliamte ERA4CS WINDSURFER urn:issn:0894-8755 https://hdl.handle.net/11250/2761403 https://doi.org/10.1175/JCLI-D-19-0540.1 cristin:1819876 Journal of Climate. 2020, 33 (2), 611–624. Copyright 2019 American Meteorological Society Journal of Climate 33 2 611-624 Journal article Peer reviewed 2020 ftunivbergen https://doi.org/10.1175/JCLI-D-19-0540.1 2023-03-14T17:41:28Z The trends in marine 10-m wind speed U10 and significant wave height Hs found in two century-long reanalyses are compared against a model-only integration. Reanalyses show spurious trends due to the assimilation of an increasing number of observations over time. The comparisons between model and reanalyses show that the areas where the discrepancies in U10 and Hs trends are greatest are also the areas where there is a marked increase in assimilated observations. Large differences in the yearly averages call into question the quality of the observations assimilated by the reanalyses, resulting in unreliable U10 and Hs trends before the 1950s. Four main regions of the world’s oceans are identified where the trends between model and reanalyses deviate strongly. These are the North Atlantic, the North Pacific, the Tasman Sea, and the western South Atlantic. The trends at +24-h lead time are markedly weaker and less correlated with the observation count. A 1985–2010 comparison with an extensive dataset of calibrated satellite altimeters shows contrasting results in Hs trends but similar U10 spatial trend distributions, with general agreement between model, reanalyses, and satellite altimeters on a broad increase in wind speed over the Southern Hemisphere. publishedVersion Article in Journal/Newspaper North Atlantic University of Bergen: Bergen Open Research Archive (BORA-UiB) Pacific Journal of Climate 33 2 611 624 |
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Open Polar |
collection |
University of Bergen: Bergen Open Research Archive (BORA-UiB) |
op_collection_id |
ftunivbergen |
language |
English |
description |
The trends in marine 10-m wind speed U10 and significant wave height Hs found in two century-long reanalyses are compared against a model-only integration. Reanalyses show spurious trends due to the assimilation of an increasing number of observations over time. The comparisons between model and reanalyses show that the areas where the discrepancies in U10 and Hs trends are greatest are also the areas where there is a marked increase in assimilated observations. Large differences in the yearly averages call into question the quality of the observations assimilated by the reanalyses, resulting in unreliable U10 and Hs trends before the 1950s. Four main regions of the world’s oceans are identified where the trends between model and reanalyses deviate strongly. These are the North Atlantic, the North Pacific, the Tasman Sea, and the western South Atlantic. The trends at +24-h lead time are markedly weaker and less correlated with the observation count. A 1985–2010 comparison with an extensive dataset of calibrated satellite altimeters shows contrasting results in Hs trends but similar U10 spatial trend distributions, with general agreement between model, reanalyses, and satellite altimeters on a broad increase in wind speed over the Southern Hemisphere. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Meucci, Alberto Young, Ian R. Aarnes, Ole Johan Breivik, Øyvind |
spellingShingle |
Meucci, Alberto Young, Ian R. Aarnes, Ole Johan Breivik, Øyvind Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters |
author_facet |
Meucci, Alberto Young, Ian R. Aarnes, Ole Johan Breivik, Øyvind |
author_sort |
Meucci, Alberto |
title |
Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters |
title_short |
Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters |
title_full |
Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters |
title_fullStr |
Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters |
title_full_unstemmed |
Comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters |
title_sort |
comparison of wind speed and wave height trends from twentieth-century models and satellite altimeters |
publisher |
American Meteorological Society |
publishDate |
2020 |
url |
https://hdl.handle.net/11250/2761403 https://doi.org/10.1175/JCLI-D-19-0540.1 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Journal of Climate 33 2 611-624 |
op_relation |
Norges forskningsråd: 256466 EC/H2020/JPI Cliamte ERA4CS WINDSURFER urn:issn:0894-8755 https://hdl.handle.net/11250/2761403 https://doi.org/10.1175/JCLI-D-19-0540.1 cristin:1819876 Journal of Climate. 2020, 33 (2), 611–624. |
op_rights |
Copyright 2019 American Meteorological Society |
op_doi |
https://doi.org/10.1175/JCLI-D-19-0540.1 |
container_title |
Journal of Climate |
container_volume |
33 |
container_issue |
2 |
container_start_page |
611 |
op_container_end_page |
624 |
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1766131932815425536 |