Surface temperature 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
Subjects:
Online Access:https://dx.doi.org/10.5446/36560
https://av.tib.eu/media/36560
id ftdatacite:10.5446/36560
record_format openpolar
spelling ftdatacite:10.5446/36560 2023-05-15T17:31:51+02:00 Surface temperature 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 https://dx.doi.org/10.5446/36560 https://av.tib.eu/media/36560 unknown Copernicus Publications Earth Sciences Climate Retrograde rotation Thought experiment Climate modeling MPI-ESM CreativeWork article ftdatacite https://doi.org/10.5446/36560 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". Monthly surface temperatures show the differences in the seasonal cycle. The most prominent differences are evident over South America and the Sahara during the Northern Hemispheric summer and western Europe and the North Atlantic during winter. The simulations also show that east-west temperature gradients over continents are reversed in the retrograde simulation (right) and are pronounced over North America and South Africa. Article in Journal/Newspaper North Atlantic DataCite Metadata Store (German National Library of Science and Technology)
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
Surface temperature 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". Monthly surface temperatures show the differences in the seasonal cycle. The most prominent differences are evident over South America and the Sahara during the Northern Hemispheric summer and western Europe and the North Atlantic during winter. The simulations also show that east-west temperature gradients over continents are reversed in the retrograde simulation (right) and are pronounced over North America and South Africa.
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 Surface temperature monthly
title_short Surface temperature monthly
title_full Surface temperature monthly
title_fullStr Surface temperature monthly
title_full_unstemmed Surface temperature monthly
title_sort surface temperature monthly
publisher Copernicus Publications
url https://dx.doi.org/10.5446/36560
https://av.tib.eu/media/36560
genre North Atlantic
genre_facet North Atlantic
op_doi https://doi.org/10.5446/36560
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