Current speed 3d monthly

Results from simulations with the coarse-resolution version of MPI-ESM performed by the RETRO team at DKRZ. The left side shows a normal (prograde) rotating earth. The right side shows a backwards (retrograde) rotating earth. The simulations are forced with pre-industrial boundary conditions. For th...

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Main Authors: Röber, Niklas, Mikolajewicz, Uwe, Ziemen, Florian, Cioni, Guido, Claussen, Martin, Fraedrich, Klaus, Heidkamp, Marvin, Hohenegger, Cathy, Jimenez De La Cuesta, Guido, Kapsch, Marie-Luise, Lemburg, Alexander, Mauritsen, Thorsten, Meraner, Katharina, Schmidt, Hauke, Six, Katharina D., Stemmler, Irene, Tamarin-Brodsky, Tali, Winkler, Alexander, Zhu, Xiuhua, Stevens, Bjorn
Format: Article in Journal/Newspaper
Language:unknown
Published: Copernicus Publications 2018
Subjects:
Online Access:https://dx.doi.org/10.5446/36551
https://av.tib.eu/media/36551
id ftdatacite:10.5446/36551
record_format openpolar
spelling ftdatacite:10.5446/36551 2023-05-15T13:44:44+02:00 Current speed 3d monthly Röber, Niklas Mikolajewicz, Uwe Ziemen, Florian Cioni, Guido Claussen, Martin Fraedrich, Klaus Heidkamp, Marvin Hohenegger, Cathy Jimenez De La Cuesta, Guido Kapsch, Marie-Luise Lemburg, Alexander Mauritsen, Thorsten Meraner, Katharina Schmidt, Hauke Six, Katharina D. Stemmler, Irene Tamarin-Brodsky, Tali Winkler, Alexander Zhu, Xiuhua Stevens, Bjorn 2018 https://dx.doi.org/10.5446/36551 https://av.tib.eu/media/36551 unknown Copernicus Publications Earth Sciences Climate Retrograde rotation Thought experiment Climate modeling MPI-ESM Research Data MediaObject article Audiovisual 2018 ftdatacite https://doi.org/10.5446/36551 2021-11-05T12:55:41Z Results from simulations with the coarse-resolution version of MPI-ESM performed by the RETRO team at DKRZ. The left side shows a normal (prograde) rotating earth. The right side shows a backwards (retrograde) rotating earth. The simulations are forced with pre-industrial boundary conditions. For the full description see the Earth System Dynamics manuscript "The climate of a retrograde rotating earth". In the retrograde simulation, the fastest currents can be observed at the American West Coast and in the Indian sector of the Antarctic Circumpolar Current. The North Atlantic Current has vanished, and only a weak boundary current at the African West coast moves water northward in the Atlantic. In the tropics, strong wave-features can be observed. Article in Journal/Newspaper Antarc* Antarctic north atlantic current North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic Indian
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Earth Sciences
Climate
Retrograde rotation
Thought experiment
Climate modeling
MPI-ESM
spellingShingle Earth Sciences
Climate
Retrograde rotation
Thought experiment
Climate modeling
MPI-ESM
Röber, Niklas
Mikolajewicz, Uwe
Ziemen, Florian
Cioni, Guido
Claussen, Martin
Fraedrich, Klaus
Heidkamp, Marvin
Hohenegger, Cathy
Jimenez De La Cuesta, Guido
Kapsch, Marie-Luise
Lemburg, Alexander
Mauritsen, Thorsten
Meraner, Katharina
Schmidt, Hauke
Six, Katharina D.
Stemmler, Irene
Tamarin-Brodsky, Tali
Winkler, Alexander
Zhu, Xiuhua
Stevens, Bjorn
Current speed 3d monthly
topic_facet Earth Sciences
Climate
Retrograde rotation
Thought experiment
Climate modeling
MPI-ESM
description Results from simulations with the coarse-resolution version of MPI-ESM performed by the RETRO team at DKRZ. The left side shows a normal (prograde) rotating earth. The right side shows a backwards (retrograde) rotating earth. The simulations are forced with pre-industrial boundary conditions. For the full description see the Earth System Dynamics manuscript "The climate of a retrograde rotating earth". In the retrograde simulation, the fastest currents can be observed at the American West Coast and in the Indian sector of the Antarctic Circumpolar Current. The North Atlantic Current has vanished, and only a weak boundary current at the African West coast moves water northward in the Atlantic. In the tropics, strong wave-features can be observed.
format Article in Journal/Newspaper
author Röber, Niklas
Mikolajewicz, Uwe
Ziemen, Florian
Cioni, Guido
Claussen, Martin
Fraedrich, Klaus
Heidkamp, Marvin
Hohenegger, Cathy
Jimenez De La Cuesta, Guido
Kapsch, Marie-Luise
Lemburg, Alexander
Mauritsen, Thorsten
Meraner, Katharina
Schmidt, Hauke
Six, Katharina D.
Stemmler, Irene
Tamarin-Brodsky, Tali
Winkler, Alexander
Zhu, Xiuhua
Stevens, Bjorn
author_facet Röber, Niklas
Mikolajewicz, Uwe
Ziemen, Florian
Cioni, Guido
Claussen, Martin
Fraedrich, Klaus
Heidkamp, Marvin
Hohenegger, Cathy
Jimenez De La Cuesta, Guido
Kapsch, Marie-Luise
Lemburg, Alexander
Mauritsen, Thorsten
Meraner, Katharina
Schmidt, Hauke
Six, Katharina D.
Stemmler, Irene
Tamarin-Brodsky, Tali
Winkler, Alexander
Zhu, Xiuhua
Stevens, Bjorn
author_sort Röber, Niklas
title Current speed 3d monthly
title_short Current speed 3d monthly
title_full Current speed 3d monthly
title_fullStr Current speed 3d monthly
title_full_unstemmed Current speed 3d monthly
title_sort current speed 3d monthly
publisher Copernicus Publications
publishDate 2018
url https://dx.doi.org/10.5446/36551
https://av.tib.eu/media/36551
geographic Antarctic
The Antarctic
Indian
geographic_facet Antarctic
The Antarctic
Indian
genre Antarc*
Antarctic
north atlantic current
North Atlantic
genre_facet Antarc*
Antarctic
north atlantic current
North Atlantic
op_doi https://doi.org/10.5446/36551
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