Zobrazeno 1 - 10
of 123
pro vyhledávání: '"Claus W. Böning"'
Autor:
Shouyi Wang, Caroline C. Ummenhofer, Delia W. Oppo, Sujata A. Murty, Patrick Wagner, Claus W. Böning, Arne Biastoch
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 14, Pp n/a-n/a (2023)
Abstract The Makassar Strait, the main passageway of the Indonesian Throughflow (ITF), is an important component of Indo‐Pacific climate through its inter‐basin redistribution of heat and freshwater. Observational studies suggest that wind‐driv
Externí odkaz:
https://doaj.org/article/0c826b3eebe346708136c6a5bb6956d1
Autor:
Baylor Fox-Kemper, Alistair Adcroft, Claus W. Böning, Eric P. Chassignet, Enrique Curchitser, Gokhan Danabasoglu, Carsten Eden, Matthew H. England, Rüdiger Gerdes, Richard J. Greatbatch, Stephen M. Griffies, Robert W. Hallberg, Emmanuel Hanert, Patrick Heimbach, Helene T. Hewitt, Christopher N. Hill, Yoshiki Komuro, Sonya Legg, Julien Le Sommer, Simona Masina, Simon J. Marsland, Stephen G. Penny, Fangli Qiao, Todd D. Ringler, Anne Marie Treguier, Hiroyuki Tsujino, Petteri Uotila, Stephen G. Yeager
Publikováno v:
Frontiers in Marine Science, Vol 6 (2019)
We revisit the challenges and prospects for ocean circulation models following Griffies et al. (2010). Over the past decade, ocean circulation models evolved through improved understanding, numerics, spatial discretization, grid configurations, param
Externí odkaz:
https://doaj.org/article/d911a83bd727495e9eacb3d3b6f71fce
Autor:
Patrick Wagner, Claus W. Böning
Publikováno v:
Ocean Science, Vol 17, Pp 1473-1487 (2021)
Strong, regional sea level trends, mainly related to basin–wide wind stress anomalies, have been observed in the western tropical Pacific over the last three decades. Analyses of regional sea level in the densely populated regions of the neighbouri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e4cecfab3558427179d42c0a2f2e8665
https://doi.org/10.5194/os-17-1473-2021
https://doi.org/10.5194/os-17-1473-2021
Publikováno v:
Ocean Science, Vol 17, Pp 1103-1113 (2021)
Regional anomalies of steric sea level are either due to redistribution of heat and freshwater anomalies or due to ocean–atmosphere buoyancy fluxes. Interannual to decadal variability in sea level across the tropical Pacific is mainly due to steric
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a8085fd8bd44a65f952fba2798b50c43
https://doi.org/10.5194/os-17-1103-2021
https://doi.org/10.5194/os-17-1103-2021
Publikováno v:
Journal of Climate. 34:1485-1502
Enhanced Southern Ocean ventilation in recent decades has been suggested to be a relevant modulator of the observed changes in ocean heat and carbon uptake. This study focuses on the Southern Ocean midlatitude ventilation changes from the 1960s to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1c4ec454535f669ad69c06f0cc24e5f4
https://doi.org/10.1175/jcli-d-19-0947.1
https://doi.org/10.1175/jcli-d-19-0947.1
Autor:
Markus Scheinert, Klaus Getzlaff, Tobias Schulzki, Siren Rühs, Arne Biastoch, Rebecca Hummels, Patricia Handmann, Franziska U. Schwarzkopf, Torge Martin, Claus W. Böning
Publikováno v:
Ocean Science, Vol 17, Pp 1177-1211 (2021)
Ocean Science, 17(5), 1177. European Geosciences Union
Ocean Science, 17(5), 1177. European Geosciences Union
A hierarchy of global 1/4∘ (ORCA025) and Atlantic Ocean 1/20∘ nested (VIKING20X) ocean–sea-ice models is described. It is shown that the eddy-rich configurations performed in hindcasts of the past 50–60 years under CORE and JRA55-do atmospher
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e3c31ee53a91b9b7128f01b81189a8a9
https://os.copernicus.org/articles/17/1177/2021/os-17-1177-2021.html
https://os.copernicus.org/articles/17/1177/2021/os-17-1177-2021.html
Autor:
Michael Dowd, Claus W. Böning, Klaus Getzlaff, Siren Rühs, Paul G. Myers, Torge Martin, Arne Biastoch, Eric C. J. Oliver
Publikováno v:
Journal of Geophysical Research: Oceans, 126(7), 1. American Geophysical Union
Deep convection and associated deep water formation are key processes for climate variability, since they impact the oceanic uptake of heat and trace gases and alter the structure and strength of the global overturning circulation. For long, deep con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0a1657acca63d586d3cfbaef41d1eb21
https://dspace.library.uu.nl/handle/1874/421492
https://dspace.library.uu.nl/handle/1874/421492
Autor:
Franziska U. Schwarzkopf, Klaus Getzlaff, Markus Scheinert, Claus W. Böning, Patrick Wagner, Siren Rühs, Arne Biastoch
A series of global ocean - sea ice model simulations is used to investigate the spatial structure and temporal variability of the sinking branch of the meridional overturning circulation (AMOC) in the subpolar North Atlantic. The experiments include
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::082db789d705a49e7f2a656025c0d431
https://doi.org/10.5194/egusphere-egu21-7789
https://doi.org/10.5194/egusphere-egu21-7789
Autor:
Eric C. J. Oliver, Siren Rühs, Michael Dowd, Arne Biastoch, Klaus Getzlaff, Paul G. Myers, Claus W. Böning
Deep convection and associated deep water formation are key processes for climate variability, since they impact the oceanic uptake of heat and trace gases and alter the structure and strength of the global overturning circulation. For long, deep con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::90fb4859d22465b080c63619f6a66feb
https://doi.org/10.5194/egusphere-egu21-10729
https://doi.org/10.5194/egusphere-egu21-10729
The Atlantic Meridional Overturning Circulation (AMOC) plays an important role for the climate system of Europe and the Arctic. It is responsible for the northward transport of warm and saline water in the upper water column and the southward transpo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::394320d75830fb84ccf9165c99829cfa
https://doi.org/10.5194/egusphere-egu21-5071
https://doi.org/10.5194/egusphere-egu21-5071