The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017

Abstract A description and assessment of the first release of the Arctic Subpolar gyre sTate Estimate (ASTE_R1), a data‐constrained ocean‐sea ice model‐data synthesis, is presented. ASTE_R1 has a nominal resolution of 1/3° and spans the period 2002–2017. The fit of the model to an extensive (O(109))...

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Autores principales: An T. Nguyen, Helen Pillar, Victor Ocaña, Arash Bigdeli, Timothy A. Smith, Patrick Heimbach
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Publicado: American Geophysical Union (AGU) 2021
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Acceso en línea:https://doaj.org/article/cf315ab640e04d349320c72cda7f5931
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spelling oai:doaj.org-article:cf315ab640e04d349320c72cda7f59312021-11-24T08:11:41ZThe Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–20171942-246610.1029/2020MS002398https://doaj.org/article/cf315ab640e04d349320c72cda7f59312021-05-01T00:00:00Zhttps://doi.org/10.1029/2020MS002398https://doaj.org/toc/1942-2466Abstract A description and assessment of the first release of the Arctic Subpolar gyre sTate Estimate (ASTE_R1), a data‐constrained ocean‐sea ice model‐data synthesis, is presented. ASTE_R1 has a nominal resolution of 1/3° and spans the period 2002–2017. The fit of the model to an extensive (O(109)) set of satellite and in situ observations was achieved through adjoint‐based nonlinear least squares optimization. The improvement of the solution compared to an unconstrained simulation is reflected in misfit reductions of 77% for Argo, 50% for satellite sea surface height, 58% for the Fram Strait mooring, 65% for Ice Tethered Profilers, and 83% for sea ice extent. Exact dynamical and kinematic consistency is a key advantage of ASTE_R1, distinguishing the state estimate from existing ocean reanalyses. Through strict adherence to conservation laws, all sources and sinks within ASTE_R1 can be accounted for, permitting meaningful analysis of closed budgets at the grid‐scale, such as contributions of horizontal and vertical convergence to the tendencies of heat and salt. ASTE_R1 thus serves as the biggest effort undertaken to date of producing a specialized Arctic ocean‐ice estimate over the 21st century. Transports of volume, heat, and freshwater are consistent with published observation‐based estimates across important Arctic Mediterranean gateways. Interannual variability and low frequency trends of freshwater and heat content are well represented in the Barents Sea, western Arctic halocline, and east subpolar North Atlantic. Systematic biases remain in ASTE_R1, including a warm bias in the Atlantic Water layer in the Arctic and deficient freshwater inputs from rivers and Greenland discharge.An T. NguyenHelen PillarVictor OcañaArash BigdeliTimothy A. SmithPatrick HeimbachAmerican Geophysical Union (AGU)articleArctic Mediterraneandata assimilationheat and freshwater exchangeocean‐sea icestate estimatesubpolar north AtlanticPhysical geographyGB3-5030OceanographyGC1-1581ENJournal of Advances in Modeling Earth Systems, Vol 13, Iss 5, Pp n/a-n/a (2021)
institution DOAJ
collection DOAJ
language EN
topic Arctic Mediterranean
data assimilation
heat and freshwater exchange
ocean‐sea ice
state estimate
subpolar north Atlantic
Physical geography
GB3-5030
Oceanography
GC1-1581
spellingShingle Arctic Mediterranean
data assimilation
heat and freshwater exchange
ocean‐sea ice
state estimate
subpolar north Atlantic
Physical geography
GB3-5030
Oceanography
GC1-1581
An T. Nguyen
Helen Pillar
Victor Ocaña
Arash Bigdeli
Timothy A. Smith
Patrick Heimbach
The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017
description Abstract A description and assessment of the first release of the Arctic Subpolar gyre sTate Estimate (ASTE_R1), a data‐constrained ocean‐sea ice model‐data synthesis, is presented. ASTE_R1 has a nominal resolution of 1/3° and spans the period 2002–2017. The fit of the model to an extensive (O(109)) set of satellite and in situ observations was achieved through adjoint‐based nonlinear least squares optimization. The improvement of the solution compared to an unconstrained simulation is reflected in misfit reductions of 77% for Argo, 50% for satellite sea surface height, 58% for the Fram Strait mooring, 65% for Ice Tethered Profilers, and 83% for sea ice extent. Exact dynamical and kinematic consistency is a key advantage of ASTE_R1, distinguishing the state estimate from existing ocean reanalyses. Through strict adherence to conservation laws, all sources and sinks within ASTE_R1 can be accounted for, permitting meaningful analysis of closed budgets at the grid‐scale, such as contributions of horizontal and vertical convergence to the tendencies of heat and salt. ASTE_R1 thus serves as the biggest effort undertaken to date of producing a specialized Arctic ocean‐ice estimate over the 21st century. Transports of volume, heat, and freshwater are consistent with published observation‐based estimates across important Arctic Mediterranean gateways. Interannual variability and low frequency trends of freshwater and heat content are well represented in the Barents Sea, western Arctic halocline, and east subpolar North Atlantic. Systematic biases remain in ASTE_R1, including a warm bias in the Atlantic Water layer in the Arctic and deficient freshwater inputs from rivers and Greenland discharge.
format article
author An T. Nguyen
Helen Pillar
Victor Ocaña
Arash Bigdeli
Timothy A. Smith
Patrick Heimbach
author_facet An T. Nguyen
Helen Pillar
Victor Ocaña
Arash Bigdeli
Timothy A. Smith
Patrick Heimbach
author_sort An T. Nguyen
title The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017
title_short The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017
title_full The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017
title_fullStr The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017
title_full_unstemmed The Arctic Subpolar Gyre sTate Estimate: Description and Assessment of a Data‐Constrained, Dynamically Consistent Ocean‐Sea Ice Estimate for 2002–2017
title_sort arctic subpolar gyre state estimate: description and assessment of a data‐constrained, dynamically consistent ocean‐sea ice estimate for 2002–2017
publisher American Geophysical Union (AGU)
publishDate 2021
url https://doaj.org/article/cf315ab640e04d349320c72cda7f5931
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