588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 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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Main Authors: Eli Tziperman, Laure Zanna, Cecile Penland
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2007
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6507
http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.419.6507 2023-05-15T17:30:49+02:00 588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM Eli Tziperman Laure Zanna Cecile Penland The Pennsylvania State University CiteSeerX Archives 2007 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6507 http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6507 http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf text 2007 ftciteseerx 2016-01-08T03:53:34Z 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. 1. Text North Atlantic Unknown
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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. 1.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Eli Tziperman
Laure Zanna
Cecile Penland
spellingShingle Eli Tziperman
Laure Zanna
Cecile Penland
588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM
author_facet Eli Tziperman
Laure Zanna
Cecile Penland
author_sort Eli Tziperman
title 588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM
title_short 588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM
title_full 588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM
title_fullStr 588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM
title_full_unstemmed 588 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 38 Nonnormal Thermohaline Circulation Dynamics in a Coupled Ocean–Atmosphere GCM
title_sort 588 journal of physical oceanography volume 38 nonnormal thermohaline circulation dynamics in a coupled ocean–atmosphere gcm
publishDate 2007
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.419.6507
http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf
genre North Atlantic
genre_facet North Atlantic
op_source http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf
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http://www.seas.harvard.edu/climate/eli/reprints/Tziperman-Zanna-Penland-2008.pdf
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