Observations of atmosphere-ocean coupling in the North Atlantic
SUMMARY An index of sea surface temperature (SST) variability, A T , is introduced that measures the difference in SST across the separated Gulf Stream in late winter. By analysing a long observational record of SST and sea-level pressure (SLP), it is shown that AT exhibits damped oscillations of de...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1082.2238 2023-05-15T16:28:16+02:00 Observations of atmosphere-ocean coupling in the North Atlantic Q J R Meteorol Soc The Pennsylvania State University CiteSeerX Archives 2001 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.2238 http://oceans.mit.edu/JohnMarshall/wp-content/uploads/2013/08/Observations-of-atmosphere-ocean-coupling-in-the-North-Atlantic_54.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.2238 http://oceans.mit.edu/JohnMarshall/wp-content/uploads/2013/08/Observations-of-atmosphere-ocean-coupling-in-the-North-Atlantic_54.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://oceans.mit.edu/JohnMarshall/wp-content/uploads/2013/08/Observations-of-atmosphere-ocean-coupling-in-the-North-Atlantic_54.pdf text 2001 ftciteseerx 2020-05-03T00:26:30Z SUMMARY An index of sea surface temperature (SST) variability, A T , is introduced that measures the difference in SST across the separated Gulf Stream in late winter. By analysing a long observational record of SST and sea-level pressure (SLP), it is shown that AT exhibits damped oscillations of decadal period, and covaries with the strength of a dipolar SLP anomaly reminiscent of the North Atlantic Oscillation (NAO). Analysis in the frequency domain shows a broad-band 'peak' at 10-20 years in A T , with a continuous decrease of power on longer time-scales. Similar spectral signatures are found in the northern part of the SLP dipole (the Greenland-Icelandic Low region) but not in its southern part (the subtropical High region), whose power increases on long time-scales. The observations are interpreted in the framework of a delayed-oscillator model in which the Ocean circulation introduces the delay, and modulates AT on decadal time-scales. The decrease of power seen on long time-scales (>25 years) in the AT index is captured by a model including wind-driven ocean circulation, and arises primarily as a passive response of the latter to the NAO forcing. Variability of the ocean's meridional overturning circulation could also play a role in modulating AT on decadal time-scales. If a small feedback of AT on the NAO pattern is introduced, the simple model can also reproduce the spectral stmctures seen in the SLP anomaly in the Greenland-Iceland region. Text Greenland Iceland North Atlantic North Atlantic oscillation Unknown Greenland |
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ftciteseerx |
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English |
description |
SUMMARY An index of sea surface temperature (SST) variability, A T , is introduced that measures the difference in SST across the separated Gulf Stream in late winter. By analysing a long observational record of SST and sea-level pressure (SLP), it is shown that AT exhibits damped oscillations of decadal period, and covaries with the strength of a dipolar SLP anomaly reminiscent of the North Atlantic Oscillation (NAO). Analysis in the frequency domain shows a broad-band 'peak' at 10-20 years in A T , with a continuous decrease of power on longer time-scales. Similar spectral signatures are found in the northern part of the SLP dipole (the Greenland-Icelandic Low region) but not in its southern part (the subtropical High region), whose power increases on long time-scales. The observations are interpreted in the framework of a delayed-oscillator model in which the Ocean circulation introduces the delay, and modulates AT on decadal time-scales. The decrease of power seen on long time-scales (>25 years) in the AT index is captured by a model including wind-driven ocean circulation, and arises primarily as a passive response of the latter to the NAO forcing. Variability of the ocean's meridional overturning circulation could also play a role in modulating AT on decadal time-scales. If a small feedback of AT on the NAO pattern is introduced, the simple model can also reproduce the spectral stmctures seen in the SLP anomaly in the Greenland-Iceland region. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Q J R Meteorol Soc |
spellingShingle |
Q J R Meteorol Soc Observations of atmosphere-ocean coupling in the North Atlantic |
author_facet |
Q J R Meteorol Soc |
author_sort |
Q J R Meteorol |
title |
Observations of atmosphere-ocean coupling in the North Atlantic |
title_short |
Observations of atmosphere-ocean coupling in the North Atlantic |
title_full |
Observations of atmosphere-ocean coupling in the North Atlantic |
title_fullStr |
Observations of atmosphere-ocean coupling in the North Atlantic |
title_full_unstemmed |
Observations of atmosphere-ocean coupling in the North Atlantic |
title_sort |
observations of atmosphere-ocean coupling in the north atlantic |
publishDate |
2001 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.2238 http://oceans.mit.edu/JohnMarshall/wp-content/uploads/2013/08/Observations-of-atmosphere-ocean-coupling-in-the-North-Atlantic_54.pdf |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Iceland North Atlantic North Atlantic oscillation |
genre_facet |
Greenland Iceland North Atlantic North Atlantic oscillation |
op_source |
http://oceans.mit.edu/JohnMarshall/wp-content/uploads/2013/08/Observations-of-atmosphere-ocean-coupling-in-the-North-Atlantic_54.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1082.2238 http://oceans.mit.edu/JohnMarshall/wp-content/uploads/2013/08/Observations-of-atmosphere-ocean-coupling-in-the-North-Atlantic_54.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766017898048913408 |