hdl:10013/epic.39677
Variability of transport through the Drake Passage and its link to the meridional pressure gradient
Sidorenko, Dmitry ORCID: https://orcid.org/0000-0001-8579-6068, Ivchenko, Vladimir, Danilov, Sergey ORCID: https://orcid.org/0000-0001-8098-182X and Schröter, Jens ORCID: https://orcid.org/0000-0002-9240-5798
;
Contact
Dmitry.Sidorenko [ at ] awi.de
Abstract
The relationship between the zonal transport across the Drake Passage and meridional pressure difference is studied by using an eddy resolving ocean state estimate simulated with the Massachusetts Institute of Technology general circulation model. The analysis is performed for monthly and yearly time series. The results show that while the meridional surface pressure difference alone can already explain a substantial part of transport variability, the pressure at 1000m gives the highest correlation. The contribution of sea surface elevation versus steric height signal are discussed.
Item Type
Conference
(Poster)
Authors
Sidorenko, Dmitry ORCID: https://orcid.org/0000-0001-8579-6068, Ivchenko, Vladimir, Danilov, Sergey ORCID: https://orcid.org/0000-0001-8098-182X and Schröter, Jens ORCID: https://orcid.org/0000-0002-9240-5798
;
Divisions
AWI Organizations > Climate Sciences > Physical Oceanography of the Polar Seas
AWI Organizations > Climate Sciences > Climate Dynamics
AWI Organizations > Climate Sciences > Climate Dynamics
Programs
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 4: Synthesis: The Earth System from a Polar Perspective > WP 4.1: Current and Future Changes of the Earth System
Publication Status
Published
Event Details
EGU General Assembly, 22 Apr 2012 - 27 Apr 2012, Vienna, Austria.
Eprint ID
30745
Cite as
Sidorenko, D.
,
Ivchenko, V.
,
Danilov, S.
and
Schröter, J.
(2012):
Variability of transport through the Drake Passage and its link to the meridional pressure gradient
,
EGU General Assembly,
Vienna, Austria,
22 April 2012 - 27 April 2012
.
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