annual

ABSTRACT In order to guide physical investigations, characterize the structure of model biases, and assess the impact of numerical and physical choices, DRAKKAR simulations are evaluated against altimetric sea-level anomalies (AVISO: 1993-present, see Poster by Penduff et al), and temperature/salini...

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Main Author: Thierry Penduff
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.424.2389
http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/2007/penduff.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.424.2389 2023-05-15T18:18:41+02:00 annual Thierry Penduff The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.424.2389 http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/2007/penduff.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.424.2389 http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/2007/penduff.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/2007/penduff.pdf Quasiglobal. 1993-2006 text ftciteseerx 2016-01-08T04:12:21Z ABSTRACT In order to guide physical investigations, characterize the structure of model biases, and assess the impact of numerical and physical choices, DRAKKAR simulations are evaluated against altimetric sea-level anomalies (AVISO: 1993-present, see Poster by Penduff et al), and temperature/salinity profiles (ENACT/ENSEMBLES: 1956-present). Model outputs are first sub-sampled like actual observations to build altimetric and hydrographic "synthetic observations". Real and synthetic observations and more integral quantities (mixed layer depth cycle, heat/salt contents, etc.) are then compared over various regions, periods, and timescales. This study presents the methods and a validation of DRAKKAR simulations with respect to hydrography Snapshot of 1/4 ° MODEL SSH + ice cover 1/4 ° GLOBAL MODEL SETUP • NEMO code (OPA9 ocean + LIM sea-ice + CFC / 14 C tracers) • Partial steps+BBL, TKE mixed layer (waves+Langmuir cells) • Advection: enstr./energy conserv. (momentum). FCT (tracers) • Isopycnal laplacian tracer mix. Biharmonic momentum mix. 1958-2004 FORCING (see Brodeau, Barnier et al) • CORE bulk formulae. Dai & Trenberth monthly runoffs. • 6-hourly ERA40 (T,q,wind) + CORE LW/SW radiative fluxes • No SST restoring. But SSS restoring (τ=36 days on 1 st level) DATA PROCESSING Validation procedure of DRAKKAR runs against altimetry and hydrography: • Collocation of model fields ( SSH(x,y,t) and T,S(x,y,z,t) ) on the observation space from various simulations. We build simulated counterparts of:-weekly 1/3°x1/3 ° SLA maps (1993-2004)- instantaneous T,S profiles (1956-2004). Flagged hydrographic observations are rejected. • Computation of derived quantities from collocated observed/simulated databases • Quantitative assessment of model skill in space and time AVISO SLA(x,y,t) database Text Sea ice Unknown Langmuir ENVELOPE(-67.150,-67.150,-66.967,-66.967)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Quasiglobal. 1993-2006
spellingShingle Quasiglobal. 1993-2006
Thierry Penduff
annual
topic_facet Quasiglobal. 1993-2006
description ABSTRACT In order to guide physical investigations, characterize the structure of model biases, and assess the impact of numerical and physical choices, DRAKKAR simulations are evaluated against altimetric sea-level anomalies (AVISO: 1993-present, see Poster by Penduff et al), and temperature/salinity profiles (ENACT/ENSEMBLES: 1956-present). Model outputs are first sub-sampled like actual observations to build altimetric and hydrographic "synthetic observations". Real and synthetic observations and more integral quantities (mixed layer depth cycle, heat/salt contents, etc.) are then compared over various regions, periods, and timescales. This study presents the methods and a validation of DRAKKAR simulations with respect to hydrography Snapshot of 1/4 ° MODEL SSH + ice cover 1/4 ° GLOBAL MODEL SETUP • NEMO code (OPA9 ocean + LIM sea-ice + CFC / 14 C tracers) • Partial steps+BBL, TKE mixed layer (waves+Langmuir cells) • Advection: enstr./energy conserv. (momentum). FCT (tracers) • Isopycnal laplacian tracer mix. Biharmonic momentum mix. 1958-2004 FORCING (see Brodeau, Barnier et al) • CORE bulk formulae. Dai & Trenberth monthly runoffs. • 6-hourly ERA40 (T,q,wind) + CORE LW/SW radiative fluxes • No SST restoring. But SSS restoring (τ=36 days on 1 st level) DATA PROCESSING Validation procedure of DRAKKAR runs against altimetry and hydrography: • Collocation of model fields ( SSH(x,y,t) and T,S(x,y,z,t) ) on the observation space from various simulations. We build simulated counterparts of:-weekly 1/3°x1/3 ° SLA maps (1993-2004)- instantaneous T,S profiles (1956-2004). Flagged hydrographic observations are rejected. • Computation of derived quantities from collocated observed/simulated databases • Quantitative assessment of model skill in space and time AVISO SLA(x,y,t) database
author2 The Pennsylvania State University CiteSeerX Archives
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author Thierry Penduff
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author_sort Thierry Penduff
title annual
title_short annual
title_full annual
title_fullStr annual
title_full_unstemmed annual
title_sort annual
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.424.2389
http://www.aviso.oceanobs.com/fileadmin/documents/OSTST/2007/penduff.pdf
long_lat ENVELOPE(-67.150,-67.150,-66.967,-66.967)
geographic Langmuir
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genre Sea ice
genre_facet Sea ice
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