Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling
© 2015, Springer-Verlag Berlin Heidelberg. The impact of the Atlantic multidecadal variability (AMV) on the wintertime atmosphere circulation is investigated using three different configurations of the Community Atmospheric Model version 5 (CAM5). Realistic SST and sea ice anomalies associated with...
Published in: | Climate Dynamics |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
eScholarship, University of California
2016
|
Subjects: | |
Online Access: | http://www.escholarship.org/uc/item/445409r9 |
id |
ftcdlib:qt445409r9 |
---|---|
record_format |
openpolar |
spelling |
ftcdlib:qt445409r9 2023-05-15T17:31:40+02:00 Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling Peings, Y Magnusdottir, G 1029 - 1047 2016-08-01 application/pdf http://www.escholarship.org/uc/item/445409r9 english eng eScholarship, University of California qt445409r9 http://www.escholarship.org/uc/item/445409r9 Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ CC-BY Peings, Y; & Magnusdottir, G. (2016). Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling. Climate Dynamics, 47(3-4), 1029 - 1047. doi:10.1007/s00382-015-2887-4. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/445409r9 article 2016 ftcdlib https://doi.org/10.1007/s00382-015-2887-4 2017-10-13T22:54:56Z © 2015, Springer-Verlag Berlin Heidelberg. The impact of the Atlantic multidecadal variability (AMV) on the wintertime atmosphere circulation is investigated using three different configurations of the Community Atmospheric Model version 5 (CAM5). Realistic SST and sea ice anomalies associated with the AMV in observations are prescribed in CAM5 (low-top model) and WACCM5 (high-top model) to assess the dependence of the results on the representation of the stratosphere. In a third experiment, the role of ocean–atmosphere feedback is investigated by coupling CAM5 to a slab-ocean model in which the AMV forcing is prescribed through oceanic heat flux anomalies. The three experiments give consistent results concerning the response of the NAO in winter, with a negative NAO signal in response to a warming of the North Atlantic ocean. This response is found in early winter when the high-top model is used, and in late winter with the low-top model. With the slab-ocean, the negative NAO response is more persistent in winter and shifted eastward over the continent due to the damping of the atmospheric response over the North Atlantic ocean. Additional experiments suggest that both tropical and extratropical SST anomalies are needed to obtain a significant modulation of the NAO, with small influence of sea ice anomalies. Warm tropical SST anomalies induce a northward shift of the ITCZ and a Rossby-wave response that is reinforced in the mid-latitudes by the extratropical SST anomalies through eddy–mean flow interactions. This modeling study supports that the positive phase of the AMV promotes the negative NAO in winter, while illustrating the impacts of the stratosphere and of the ocean–atmosphere feedbacks in the spatial pattern and timing of this response. Article in Journal/Newspaper North Atlantic Sea ice University of California: eScholarship Climate Dynamics 47 3-4 1029 1047 |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
English |
description |
© 2015, Springer-Verlag Berlin Heidelberg. The impact of the Atlantic multidecadal variability (AMV) on the wintertime atmosphere circulation is investigated using three different configurations of the Community Atmospheric Model version 5 (CAM5). Realistic SST and sea ice anomalies associated with the AMV in observations are prescribed in CAM5 (low-top model) and WACCM5 (high-top model) to assess the dependence of the results on the representation of the stratosphere. In a third experiment, the role of ocean–atmosphere feedback is investigated by coupling CAM5 to a slab-ocean model in which the AMV forcing is prescribed through oceanic heat flux anomalies. The three experiments give consistent results concerning the response of the NAO in winter, with a negative NAO signal in response to a warming of the North Atlantic ocean. This response is found in early winter when the high-top model is used, and in late winter with the low-top model. With the slab-ocean, the negative NAO response is more persistent in winter and shifted eastward over the continent due to the damping of the atmospheric response over the North Atlantic ocean. Additional experiments suggest that both tropical and extratropical SST anomalies are needed to obtain a significant modulation of the NAO, with small influence of sea ice anomalies. Warm tropical SST anomalies induce a northward shift of the ITCZ and a Rossby-wave response that is reinforced in the mid-latitudes by the extratropical SST anomalies through eddy–mean flow interactions. This modeling study supports that the positive phase of the AMV promotes the negative NAO in winter, while illustrating the impacts of the stratosphere and of the ocean–atmosphere feedbacks in the spatial pattern and timing of this response. |
format |
Article in Journal/Newspaper |
author |
Peings, Y Magnusdottir, G |
spellingShingle |
Peings, Y Magnusdottir, G Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling |
author_facet |
Peings, Y Magnusdottir, G |
author_sort |
Peings, Y |
title |
Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling |
title_short |
Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling |
title_full |
Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling |
title_fullStr |
Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling |
title_full_unstemmed |
Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling |
title_sort |
wintertime atmospheric response to atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling |
publisher |
eScholarship, University of California |
publishDate |
2016 |
url |
http://www.escholarship.org/uc/item/445409r9 |
op_coverage |
1029 - 1047 |
genre |
North Atlantic Sea ice |
genre_facet |
North Atlantic Sea ice |
op_source |
Peings, Y; & Magnusdottir, G. (2016). Wintertime atmospheric response to Atlantic multidecadal variability: effect of stratospheric representation and ocean–atmosphere coupling. Climate Dynamics, 47(3-4), 1029 - 1047. doi:10.1007/s00382-015-2887-4. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/445409r9 |
op_relation |
qt445409r9 http://www.escholarship.org/uc/item/445409r9 |
op_rights |
Attribution (CC BY): http://creativecommons.org/licenses/by/3.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1007/s00382-015-2887-4 |
container_title |
Climate Dynamics |
container_volume |
47 |
container_issue |
3-4 |
container_start_page |
1029 |
op_container_end_page |
1047 |
_version_ |
1766129344345800704 |