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dc.contributor.authorLei Liu
dc.contributor.authorHuijie Xue
dc.date.accessioned2023-04-12T18:32:56Z
dc.date.available2023-04-12T18:32:56Z
dc.date.copyright2022/10/04
dc.date.issued2022
dc.identifier.otherJPO-D-21-0183.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289857
dc.description.abstractObservational surface data are utilized to reconstruct the subsurface density and geostrophic velocity fields via the “interior + surface quasigeostrophic” (isQG) method in a subdomain of the Antarctic Circumpolar Current (ACC). The input variables include the satellite-derived sea surface height (SSH), satellite-derived sea surface temperature (SST), satellite-derived or Argo-based sea surface salinity (SSS), and a monthly estimate of the stratification. The density reconstruction is assessed against a newly released high-resolution in situ dataset that is collected by a southern elephant seal. The results show that the observed mesoscale structures are reasonably reconstructed. In the Argo-SSS-based experiment, pattern correlations between the reconstructed and observed density mostly exceed 0.8 in the upper 300 m. Uncertainties in the SSS products notably influence the isQG performance, and the Argo-SSS-based experiment yields better density reconstruction than the satellite-SSS-based one. Through the two-dimensional (2D) omega equation, we further employ the isQG reconstructions to diagnose the upper-ocean vertical velocities (denoted
dc.publisherAmerican Meteorological Society
dc.titleEstimating the Ocean Interior from Satellite Observations in the Kerguelen Area (Southern Ocean): A Combined Investigation Using High-Resolution CTD Data from Animal-Borne Instruments
dc.typeJournal Paper
dc.journal.volume52
dc.journal.issue10
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-21-0183.1
dc.journal.fristpage2463
dc.journal.lastpage2478
dc.page2463–2478
dc.treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 010
dc.contenttypeFulltext


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