Ocean Reanalyses

Ocean reanalyses are becoming increasingly available and useful, and may eventually attract a similar applications base as atmospheric reanalyses. Here we look at how they are being evaluated against both assimilated and independent data, and emphasise that circulation and transport estimates are cr...

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Other Authors: Haines, Keith (authoraut)
Format: Book Part
Language:English
Subjects:
Ora
Online Access:https://doi.org/10.17125/gov2018.ch19
http://purl.flvc.org/fsu/fd/FSU_libsubv1_scholarship_submission_1536244792_a60d1e66
http://fsu.digital.flvc.org/islandora/object/fsu%3A602122/datastream/TN/view/Ocean%20Reanalyses.jpg
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spelling ftfloridastunidc:oai:fsu.digital.flvc.org:fsu_602122 2023-05-15T18:18:37+02:00 Ocean Reanalyses Haines, Keith (authoraut) 1 online resource computer application/pdf https://doi.org/10.17125/gov2018.ch19 http://purl.flvc.org/fsu/fd/FSU_libsubv1_scholarship_submission_1536244792_a60d1e66 http://fsu.digital.flvc.org/islandora/object/fsu%3A602122/datastream/TN/view/Ocean%20Reanalyses.jpg English eng eng New Frontiers in Operational Oceanography Text book part ftfloridastunidc https://doi.org/10.17125/gov2018.ch19 2020-08-10T18:26:41Z Ocean reanalyses are becoming increasingly available and useful, and may eventually attract a similar applications base as atmospheric reanalyses. Here we look at how they are being evaluated against both assimilated and independent data, and emphasise that circulation and transport estimates are critical. The Ocean Reanalysis Intercomparison project, ORA-IP, has been comparing many products for consistency on a regional and global basis, including ocean heat content, air-sea fluxes, and recently polar properties including sea ice. The Atlantic meridional overturning circulation as measured by the RAPID array at 26N, is now a challenging new target for simulation. This chapter shows that reanalyses may represent interior ocean basin circulations well (better than free-running models) but they still fail to consistently constrain boundary currents, where most meridional heat transport takes place. There is new work ongoing to try to physically interpret observation increments in reanalysis products, and to look at how to best develop long period reanalysis in earlier years when ocean observations were scarce. Finally, we look at new coupled ocean-atmosphere reanalysis that, by always maintaining a coupled ocean-atmospheric boundary layer, may lead to reduced assimilation increments and air-sea fluxes across domains. Terms and Conditions: Readers may view, browse, and/or download material for temporary copying purposes only, provided these uses are for noncommercial personal purposes. Except as provided by law, this material may not be further reproduced, distributed, transmitted, modified, adapted, performed, displayed, published, or sold in whole or in part, without prior written permission from GODAE OceanView. Book Part Sea ice Florida State University Digital Library (FSUDL) Ora ENVELOPE(7.517,7.517,62.581,62.581)
institution Open Polar
collection Florida State University Digital Library (FSUDL)
op_collection_id ftfloridastunidc
language English
description Ocean reanalyses are becoming increasingly available and useful, and may eventually attract a similar applications base as atmospheric reanalyses. Here we look at how they are being evaluated against both assimilated and independent data, and emphasise that circulation and transport estimates are critical. The Ocean Reanalysis Intercomparison project, ORA-IP, has been comparing many products for consistency on a regional and global basis, including ocean heat content, air-sea fluxes, and recently polar properties including sea ice. The Atlantic meridional overturning circulation as measured by the RAPID array at 26N, is now a challenging new target for simulation. This chapter shows that reanalyses may represent interior ocean basin circulations well (better than free-running models) but they still fail to consistently constrain boundary currents, where most meridional heat transport takes place. There is new work ongoing to try to physically interpret observation increments in reanalysis products, and to look at how to best develop long period reanalysis in earlier years when ocean observations were scarce. Finally, we look at new coupled ocean-atmosphere reanalysis that, by always maintaining a coupled ocean-atmospheric boundary layer, may lead to reduced assimilation increments and air-sea fluxes across domains. Terms and Conditions: Readers may view, browse, and/or download material for temporary copying purposes only, provided these uses are for noncommercial personal purposes. Except as provided by law, this material may not be further reproduced, distributed, transmitted, modified, adapted, performed, displayed, published, or sold in whole or in part, without prior written permission from GODAE OceanView.
author2 Haines, Keith (authoraut)
format Book Part
title Ocean Reanalyses
spellingShingle Ocean Reanalyses
title_short Ocean Reanalyses
title_full Ocean Reanalyses
title_fullStr Ocean Reanalyses
title_full_unstemmed Ocean Reanalyses
title_sort ocean reanalyses
url https://doi.org/10.17125/gov2018.ch19
http://purl.flvc.org/fsu/fd/FSU_libsubv1_scholarship_submission_1536244792_a60d1e66
http://fsu.digital.flvc.org/islandora/object/fsu%3A602122/datastream/TN/view/Ocean%20Reanalyses.jpg
long_lat ENVELOPE(7.517,7.517,62.581,62.581)
geographic Ora
geographic_facet Ora
genre Sea ice
genre_facet Sea ice
op_relation New Frontiers in Operational Oceanography
op_doi https://doi.org/10.17125/gov2018.ch19
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