Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability

The simulated impact of the Atlantic Meridional Overturning Circulation (AMOC) on the low frequency variability of the Arctic Surface Air temperature (SAT) and sea-ice extent is studied with a 1000 year-long segment of a control simulation of GFDL CM2.1 climate model. The simulated AMOC variations i...

Full description

Bibliographic Details
Main Authors: Salil Mahajan, Rong Zhang, Thomas L. Delworth
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.224.5071
http://www.gfdl.gov/cms-filesystem-action/user_files/td/amoc_and_arctic_jcli_revision2.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.224.5071
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.224.5071 2023-05-15T14:33:14+02:00 Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability Salil Mahajan Rong Zhang Thomas L. Delworth The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.224.5071 http://www.gfdl.gov/cms-filesystem-action/user_files/td/amoc_and_arctic_jcli_revision2.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.224.5071 http://www.gfdl.gov/cms-filesystem-action/user_files/td/amoc_and_arctic_jcli_revision2.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.gfdl.gov/cms-filesystem-action/user_files/td/amoc_and_arctic_jcli_revision2.pdf text ftciteseerx 2016-01-07T18:25:55Z The simulated impact of the Atlantic Meridional Overturning Circulation (AMOC) on the low frequency variability of the Arctic Surface Air temperature (SAT) and sea-ice extent is studied with a 1000 year-long segment of a control simulation of GFDL CM2.1 climate model. The simulated AMOC variations in the control simulation are found to be significantly anti-correlated with the Arctic sea-ice extent anomalies and significantly correlated with the Arctic SAT anomalies on decadal timescales in the Atlantic sector of the Arctic. The maximum anti-correlation with the Arctic sea-ice extent and the maximum correlation with the Arctic SAT occur when the AMOC Index leads by one year. An intensification of the AMOC is associated with a sea-ice decline in the Labrador, Greenland and Barents Seas in the control simulation, with the largest change occurring in the winter. The recent declining trend in the satellite observed sea-ice extent also shows a similar pattern in the Atlantic sector of the Arctic in the winter, suggesting the possibility of a role of the AMOC in the recent Arctic sea-ice decline in addition to anthropogenic greenhouse gas induced warming. However, in the summer, the simulated sea-ice response to the AMOC in the Pacific sector of the Arctic is much weaker than the observed declining trend, indicating a stronger role for other climate forcings or variability in the recently observed summer sea-ice decline in the Chukchi, Beaufort, East Siberian and Laptev Seas. Text Arctic Chukchi Greenland laptev Sea ice Unknown Arctic Greenland Pacific
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description The simulated impact of the Atlantic Meridional Overturning Circulation (AMOC) on the low frequency variability of the Arctic Surface Air temperature (SAT) and sea-ice extent is studied with a 1000 year-long segment of a control simulation of GFDL CM2.1 climate model. The simulated AMOC variations in the control simulation are found to be significantly anti-correlated with the Arctic sea-ice extent anomalies and significantly correlated with the Arctic SAT anomalies on decadal timescales in the Atlantic sector of the Arctic. The maximum anti-correlation with the Arctic sea-ice extent and the maximum correlation with the Arctic SAT occur when the AMOC Index leads by one year. An intensification of the AMOC is associated with a sea-ice decline in the Labrador, Greenland and Barents Seas in the control simulation, with the largest change occurring in the winter. The recent declining trend in the satellite observed sea-ice extent also shows a similar pattern in the Atlantic sector of the Arctic in the winter, suggesting the possibility of a role of the AMOC in the recent Arctic sea-ice decline in addition to anthropogenic greenhouse gas induced warming. However, in the summer, the simulated sea-ice response to the AMOC in the Pacific sector of the Arctic is much weaker than the observed declining trend, indicating a stronger role for other climate forcings or variability in the recently observed summer sea-ice decline in the Chukchi, Beaufort, East Siberian and Laptev Seas.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Salil Mahajan
Rong Zhang
Thomas L. Delworth
spellingShingle Salil Mahajan
Rong Zhang
Thomas L. Delworth
Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability
author_facet Salil Mahajan
Rong Zhang
Thomas L. Delworth
author_sort Salil Mahajan
title Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability
title_short Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability
title_full Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability
title_fullStr Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability
title_full_unstemmed Generated using version 3.0 of the official AMS L ATEX template Impact of the Atlantic Meridional Overturning Circulation (AMOC) on Arctic Surface Air Temperature and Sea-Ice Variability
title_sort generated using version 3.0 of the official ams l atex template impact of the atlantic meridional overturning circulation (amoc) on arctic surface air temperature and sea-ice variability
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.224.5071
http://www.gfdl.gov/cms-filesystem-action/user_files/td/amoc_and_arctic_jcli_revision2.pdf
geographic Arctic
Greenland
Pacific
geographic_facet Arctic
Greenland
Pacific
genre Arctic
Chukchi
Greenland
laptev
Sea ice
genre_facet Arctic
Chukchi
Greenland
laptev
Sea ice
op_source http://www.gfdl.gov/cms-filesystem-action/user_files/td/amoc_and_arctic_jcli_revision2.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.224.5071
http://www.gfdl.gov/cms-filesystem-action/user_files/td/amoc_and_arctic_jcli_revision2.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766306498863955968