On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies
The Gravity Recovery and Climate Experiment provides monthly estimates of the Earths gravity field. Temporal changes in the gravitational field are associated with mass movement. Over the ocean these fluctuations are primarily due to changes in atmosphere and ocean circulation associated with ocean...
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ftawi:oai:epic.awi.de:21568 2024-09-09T20:09:30+00:00 On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies Böning, Carmen Zotnicki, V. Fetter, A. Timmermann, Ralph Danilov, Sergey Schröter, Jens 2009 https://epic.awi.de/id/eprint/21568/ https://hdl.handle.net/10013/epic.33913 unknown Böning, C. , Zotnicki, V. , Fetter, A. , Timmermann, R. , Danilov, S. orcid:0000-0001-8098-182X and Schröter, J. orcid:0000-0002-9240-5798 (2009) On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies , 2009 AGU Fall Meeting18 December San Francisco, California, USA. . hdl:10013/epic.33913 EPIC32009 AGU Fall Meeting18 December San Francisco, California, USA., 14 Conference notRev 2009 ftawi 2024-06-24T04:01:54Z The Gravity Recovery and Climate Experiment provides monthly estimates of the Earths gravity field. Temporal changes in the gravitational field are associated with mass movement. Over the ocean these fluctuations are primarily due to changes in atmosphere and ocean circulation associated with ocean bottom pressure (OBP). In this study the ability of GRACE to observe circulation variability in the Southern Ocean is investigated. Conference Object Southern Ocean Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Southern Ocean |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
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description |
The Gravity Recovery and Climate Experiment provides monthly estimates of the Earths gravity field. Temporal changes in the gravitational field are associated with mass movement. Over the ocean these fluctuations are primarily due to changes in atmosphere and ocean circulation associated with ocean bottom pressure (OBP). In this study the ability of GRACE to observe circulation variability in the Southern Ocean is investigated. |
format |
Conference Object |
author |
Böning, Carmen Zotnicki, V. Fetter, A. Timmermann, Ralph Danilov, Sergey Schröter, Jens |
spellingShingle |
Böning, Carmen Zotnicki, V. Fetter, A. Timmermann, Ralph Danilov, Sergey Schröter, Jens On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies |
author_facet |
Böning, Carmen Zotnicki, V. Fetter, A. Timmermann, Ralph Danilov, Sergey Schröter, Jens |
author_sort |
Böning, Carmen |
title |
On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies |
title_short |
On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies |
title_full |
On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies |
title_fullStr |
On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies |
title_full_unstemmed |
On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies |
title_sort |
on the representation of southern ocean mass variability in grace-derived ocean bottom pressure anomalies |
publishDate |
2009 |
url |
https://epic.awi.de/id/eprint/21568/ https://hdl.handle.net/10013/epic.33913 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
EPIC32009 AGU Fall Meeting18 December San Francisco, California, USA., 14 |
op_relation |
Böning, C. , Zotnicki, V. , Fetter, A. , Timmermann, R. , Danilov, S. orcid:0000-0001-8098-182X and Schröter, J. orcid:0000-0002-9240-5798 (2009) On the representation of Southern Ocean mass variability in GRACE-derived ocean bottom pressure anomalies , 2009 AGU Fall Meeting18 December San Francisco, California, USA. . hdl:10013/epic.33913 |
_version_ |
1809943668270825472 |