Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM
Using the GFDL coupled atmosphere–ocean general circulation model CM2.1, the transient amplification of thermohaline circulation (THC) anomalies due to its nonnormal dynamics is studied. A reduced space based on empirical orthogonal functions (EOFs) of temperature and salinity anomaly fields in the...
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American Meteorological Society
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ftharvardudash:oai:dash.harvard.edu:1/3445050 2023-05-15T17:30:54+02:00 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM Tziperman, Eli Zanna, Laure Penland, Cecile 2008 application/pdf http://nrs.harvard.edu/urn-3:HUL.InstRepos:3445050 https://doi.org/10.1175/2007JPO3769.1 en_US eng American Meteorological Society doi:10.1175/2007JPO3769.1 http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf Journal of Physical Oceanography Tziperman, Eli, Laure Zanna, and Cecile Penland. 2008. Nonnormal thermohaline circulation dynamics in a coupled ocean-atmosphere GCM. Journal of Physical Oceanography 38(3): 588-604. 0022-3670 http://nrs.harvard.edu/urn-3:HUL.InstRepos:3445050 Journal Article 2008 ftharvardudash https://doi.org/10.1175/2007JPO3769.1 2022-04-04T12:36:40Z Using the GFDL coupled atmosphere–ocean general circulation model CM2.1, the transient amplification of thermohaline circulation (THC) anomalies due to its nonnormal dynamics is studied. A reduced space based on empirical orthogonal functions (EOFs) of temperature and salinity anomaly fields in the North Atlantic is constructed. Under the assumption that the dynamics of this reduced space is linear, the propagator of the system is then evaluated and the transient growth of THC anomalies analyzed. Although the linear dynamics are stable, such that any initial perturbation eventually decays, nonnormal effects are found to result in a significant transient growth of temperature, salinity, and THC anomalies. The growth time scale for these anomalies is between 5 and 10 yr, providing an estimate of the predictability time of the North Atlantic THC in this model. There are indications that these results are merely a lower bound on the nonnormality of THC dynamics in the present coupled GCM. This seems to suggest that such nonnormal effects should be seriously considered if the predictability of the THC is to be quantitatively evaluated from models or observations. The methodology presented here may be used to produce initial perturbations to the ocean state that may result in a stricter estimate of ocean and THC predictability than the common procedure of initializing with an identical ocean state and a perturbed atmosphere. Earth and Planetary Sciences Version of Record Article in Journal/Newspaper North Atlantic Harvard University: DASH - Digital Access to Scholarship at Harvard Journal of Physical Oceanography 38 3 588 604 |
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Open Polar |
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Harvard University: DASH - Digital Access to Scholarship at Harvard |
op_collection_id |
ftharvardudash |
language |
English |
description |
Using the GFDL coupled atmosphere–ocean general circulation model CM2.1, the transient amplification of thermohaline circulation (THC) anomalies due to its nonnormal dynamics is studied. A reduced space based on empirical orthogonal functions (EOFs) of temperature and salinity anomaly fields in the North Atlantic is constructed. Under the assumption that the dynamics of this reduced space is linear, the propagator of the system is then evaluated and the transient growth of THC anomalies analyzed. Although the linear dynamics are stable, such that any initial perturbation eventually decays, nonnormal effects are found to result in a significant transient growth of temperature, salinity, and THC anomalies. The growth time scale for these anomalies is between 5 and 10 yr, providing an estimate of the predictability time of the North Atlantic THC in this model. There are indications that these results are merely a lower bound on the nonnormality of THC dynamics in the present coupled GCM. This seems to suggest that such nonnormal effects should be seriously considered if the predictability of the THC is to be quantitatively evaluated from models or observations. The methodology presented here may be used to produce initial perturbations to the ocean state that may result in a stricter estimate of ocean and THC predictability than the common procedure of initializing with an identical ocean state and a perturbed atmosphere. Earth and Planetary Sciences Version of Record |
format |
Article in Journal/Newspaper |
author |
Tziperman, Eli Zanna, Laure Penland, Cecile |
spellingShingle |
Tziperman, Eli Zanna, Laure Penland, Cecile Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM |
author_facet |
Tziperman, Eli Zanna, Laure Penland, Cecile |
author_sort |
Tziperman, Eli |
title |
Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM |
title_short |
Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM |
title_full |
Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM |
title_fullStr |
Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM |
title_full_unstemmed |
Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM |
title_sort |
nonnormal thermohaline circulation dynamics in a coupled ocean–atmosphere gcm |
publisher |
American Meteorological Society |
publishDate |
2008 |
url |
http://nrs.harvard.edu/urn-3:HUL.InstRepos:3445050 https://doi.org/10.1175/2007JPO3769.1 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
doi:10.1175/2007JPO3769.1 http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf Journal of Physical Oceanography Tziperman, Eli, Laure Zanna, and Cecile Penland. 2008. Nonnormal thermohaline circulation dynamics in a coupled ocean-atmosphere GCM. Journal of Physical Oceanography 38(3): 588-604. 0022-3670 http://nrs.harvard.edu/urn-3:HUL.InstRepos:3445050 |
op_doi |
https://doi.org/10.1175/2007JPO3769.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
38 |
container_issue |
3 |
container_start_page |
588 |
op_container_end_page |
604 |
_version_ |
1766128030063788032 |