Impact of combining GRACE and GOCE gravity data on ocean circulation estimates
In this work we examine the impact of assimilation of multi-mission-altimeter data and the GRACE/GOCE gravity fields into the finite element ocean model (FEOM), with the focus on the Southern Ocean circulation. In order to do so, we use the geodetic approach for obtaining the dynamical ocean topogra...
Main Authors: | , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2011
|
Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/24592/ https://doi.org/10.5194/osd-8-1535-2011 https://hdl.handle.net/10013/epic.39481 |
id |
ftawi:oai:epic.awi.de:24592 |
---|---|
record_format |
openpolar |
spelling |
ftawi:oai:epic.awi.de:24592 2024-09-15T18:37:13+00:00 Impact of combining GRACE and GOCE gravity data on ocean circulation estimates Janjic Pfander, Tijana Schröter, Jens Savcenko, R. Bosch, W. Albertella, A. Rummel, R. Klatt, Olaf 2011 https://epic.awi.de/id/eprint/24592/ https://doi.org/10.5194/osd-8-1535-2011 https://hdl.handle.net/10013/epic.39481 unknown Janjic Pfander, T. , Schröter, J. orcid:0000-0002-9240-5798 , Savcenko, R. , Bosch, W. , Albertella, A. , Rummel, R. and Klatt, O. (2011) Impact of combining GRACE and GOCE gravity data on ocean circulation estimates , Ocean Sci. Discuss, 8 , pp. 1535-1573 . doi:10.5194/osd-8-1535-2011 <https://doi.org/10.5194/osd-8-1535-2011> , hdl:10013/epic.39481 EPIC3Ocean Sci. Discuss, 8, pp. 1535-1573 Article notRev 2011 ftawi https://doi.org/10.5194/osd-8-1535-2011 2024-06-24T04:02:42Z In this work we examine the impact of assimilation of multi-mission-altimeter data and the GRACE/GOCE gravity fields into the finite element ocean model (FEOM), with the focus on the Southern Ocean circulation. In order to do so, we use the geodetic approach for obtaining the dynamical ocean topography (DOT), that combines the multi-mission-altimeter data and the GRACE/GOCE gravity fields, and requires that both fields be spectrally consistent. The spectral consistency is achieved by filtering of the sea surface height and the geoid using profile approach. Combining the GRACE and GOCE data, a considerably shorter filter length resolving more DOT details can be used. In order to specify the spectrally consistent geodetic DOT we applied the Jekeli-Wahr filter corresponding to 241 km, 121 km, 97 km and 81 km halfwidths for the GRACE/GOCE based gravity field model GOCO01S and to the sea surface. More realistic features of the ocean assimilation were obtained in the Weddel gyre area due to increased resolution of the data fields, particularly for temperature field at the 800 m depth compared to Argo data. Article in Journal/Newspaper Southern Ocean Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
In this work we examine the impact of assimilation of multi-mission-altimeter data and the GRACE/GOCE gravity fields into the finite element ocean model (FEOM), with the focus on the Southern Ocean circulation. In order to do so, we use the geodetic approach for obtaining the dynamical ocean topography (DOT), that combines the multi-mission-altimeter data and the GRACE/GOCE gravity fields, and requires that both fields be spectrally consistent. The spectral consistency is achieved by filtering of the sea surface height and the geoid using profile approach. Combining the GRACE and GOCE data, a considerably shorter filter length resolving more DOT details can be used. In order to specify the spectrally consistent geodetic DOT we applied the Jekeli-Wahr filter corresponding to 241 km, 121 km, 97 km and 81 km halfwidths for the GRACE/GOCE based gravity field model GOCO01S and to the sea surface. More realistic features of the ocean assimilation were obtained in the Weddel gyre area due to increased resolution of the data fields, particularly for temperature field at the 800 m depth compared to Argo data. |
format |
Article in Journal/Newspaper |
author |
Janjic Pfander, Tijana Schröter, Jens Savcenko, R. Bosch, W. Albertella, A. Rummel, R. Klatt, Olaf |
spellingShingle |
Janjic Pfander, Tijana Schröter, Jens Savcenko, R. Bosch, W. Albertella, A. Rummel, R. Klatt, Olaf Impact of combining GRACE and GOCE gravity data on ocean circulation estimates |
author_facet |
Janjic Pfander, Tijana Schröter, Jens Savcenko, R. Bosch, W. Albertella, A. Rummel, R. Klatt, Olaf |
author_sort |
Janjic Pfander, Tijana |
title |
Impact of combining GRACE and GOCE gravity data on ocean circulation estimates |
title_short |
Impact of combining GRACE and GOCE gravity data on ocean circulation estimates |
title_full |
Impact of combining GRACE and GOCE gravity data on ocean circulation estimates |
title_fullStr |
Impact of combining GRACE and GOCE gravity data on ocean circulation estimates |
title_full_unstemmed |
Impact of combining GRACE and GOCE gravity data on ocean circulation estimates |
title_sort |
impact of combining grace and goce gravity data on ocean circulation estimates |
publishDate |
2011 |
url |
https://epic.awi.de/id/eprint/24592/ https://doi.org/10.5194/osd-8-1535-2011 https://hdl.handle.net/10013/epic.39481 |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
EPIC3Ocean Sci. Discuss, 8, pp. 1535-1573 |
op_relation |
Janjic Pfander, T. , Schröter, J. orcid:0000-0002-9240-5798 , Savcenko, R. , Bosch, W. , Albertella, A. , Rummel, R. and Klatt, O. (2011) Impact of combining GRACE and GOCE gravity data on ocean circulation estimates , Ocean Sci. Discuss, 8 , pp. 1535-1573 . doi:10.5194/osd-8-1535-2011 <https://doi.org/10.5194/osd-8-1535-2011> , hdl:10013/epic.39481 |
op_doi |
https://doi.org/10.5194/osd-8-1535-2011 |
_version_ |
1810481575275528192 |