DNSC08 mean sea surface and mean dynamic topography models

The Danish National Space Center data set DNSC08 mean sea surface (MSS) is a new enhanced mapping of the mean sea surface height of the worlds oceans, derived from a combination of 12 years of satellite altimetry from a total of eight different satellites covering the period 1993–2004. It is the fir...

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Published in:Journal of Geophysical Research
Main Authors: Andersen, O., Knudsen, P.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2009
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834079
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_1834079 2023-05-15T15:08:38+02:00 DNSC08 mean sea surface and mean dynamic topography models Andersen, O. Knudsen, P. 2009 https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834079 unknown info:eu-repo/semantics/altIdentifier/doi/10.1029/2008jc005179 info:eu-repo/semantics/altIdentifier/pissn/0148-0227 https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834079 Journal of Geophysical Research info:eu-repo/semantics/article 2009 ftgfzpotsdam https://doi.org/10.1029/2008jc005179 2022-09-14T05:55:03Z The Danish National Space Center data set DNSC08 mean sea surface (MSS) is a new enhanced mapping of the mean sea surface height of the worlds oceans, derived from a combination of 12 years of satellite altimetry from a total of eight different satellites covering the period 1993–2004. It is the first global MSS without a polar gap including all of the Arctic Ocean by including laser altimetry from the ICESat mission. The mean dynamic topography (MDT) is the quantity that bridges the geoid and the mean sea surface constraining large-scale ocean circulation. Here we present a new high-resolution 1 min global MDT called DNSC08 MDT derived from the slightly smoothed difference between the DNSC08 MSS and the EGM2008 geoid. The derivation and quality control of the new DNSC08 MSS and DNSC08 MDT is presented in this paper along with suggestions for time period standardization of the MSS and MDT models. This way a consistent modeling of the interannual sea level variability is carried out before different MSS and MDT models are compared. Altimetric derived physical MSS can be converted into an “inverse barometer corrected MSS” by correcting the altimeter range for the inverse barometer effect of the atmosphere on the sea surface height. It is demonstrated that it is important to choose the right version of the MSS when comparing with hydrodynamic models and GPS measured tide gauges. Article in Journal/Newspaper Arctic Arctic Ocean GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Arctic Ocean Journal of Geophysical Research 114 C11
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language unknown
description The Danish National Space Center data set DNSC08 mean sea surface (MSS) is a new enhanced mapping of the mean sea surface height of the worlds oceans, derived from a combination of 12 years of satellite altimetry from a total of eight different satellites covering the period 1993–2004. It is the first global MSS without a polar gap including all of the Arctic Ocean by including laser altimetry from the ICESat mission. The mean dynamic topography (MDT) is the quantity that bridges the geoid and the mean sea surface constraining large-scale ocean circulation. Here we present a new high-resolution 1 min global MDT called DNSC08 MDT derived from the slightly smoothed difference between the DNSC08 MSS and the EGM2008 geoid. The derivation and quality control of the new DNSC08 MSS and DNSC08 MDT is presented in this paper along with suggestions for time period standardization of the MSS and MDT models. This way a consistent modeling of the interannual sea level variability is carried out before different MSS and MDT models are compared. Altimetric derived physical MSS can be converted into an “inverse barometer corrected MSS” by correcting the altimeter range for the inverse barometer effect of the atmosphere on the sea surface height. It is demonstrated that it is important to choose the right version of the MSS when comparing with hydrodynamic models and GPS measured tide gauges.
format Article in Journal/Newspaper
author Andersen, O.
Knudsen, P.
spellingShingle Andersen, O.
Knudsen, P.
DNSC08 mean sea surface and mean dynamic topography models
author_facet Andersen, O.
Knudsen, P.
author_sort Andersen, O.
title DNSC08 mean sea surface and mean dynamic topography models
title_short DNSC08 mean sea surface and mean dynamic topography models
title_full DNSC08 mean sea surface and mean dynamic topography models
title_fullStr DNSC08 mean sea surface and mean dynamic topography models
title_full_unstemmed DNSC08 mean sea surface and mean dynamic topography models
title_sort dnsc08 mean sea surface and mean dynamic topography models
publishDate 2009
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834079
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
genre_facet Arctic
Arctic Ocean
op_source Journal of Geophysical Research
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2008jc005179
info:eu-repo/semantics/altIdentifier/pissn/0148-0227
https://gfzpublic.gfz-potsdam.de/pubman/item/item_1834079
op_doi https://doi.org/10.1029/2008jc005179
container_title Journal of Geophysical Research
container_volume 114
container_issue C11
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