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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Published in:Journal of Physical Oceanography
Main Authors: Tziperman, E, Zanna, L, Penland, C
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.1175/2007JPO3769.1
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:cc981a14-7adf-4d96-ac6d-bcf0559d422d 2023-05-15T17:30:54+02:00 Nonnormal thermohaline circulation dynamics in a coupled ocean-atmosphere GCM Tziperman, E Zanna, L Penland, C 2016-07-29 https://doi.org/10.1175/2007JPO3769.1 https://ora.ox.ac.uk/objects/uuid:cc981a14-7adf-4d96-ac6d-bcf0559d422d eng eng doi:10.1175/2007JPO3769.1 https://ora.ox.ac.uk/objects/uuid:cc981a14-7adf-4d96-ac6d-bcf0559d422d https://doi.org/10.1175/2007JPO3769.1 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1175/2007JPO3769.1 2022-06-28T20:24:08Z 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. © 2008 American Meteorological Society. Article in Journal/Newspaper North Atlantic ORA - Oxford University Research Archive Journal of Physical Oceanography 38 3 588 604
institution Open Polar
collection ORA - Oxford University Research Archive
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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. © 2008 American Meteorological Society.
format Article in Journal/Newspaper
author Tziperman, E
Zanna, L
Penland, C
spellingShingle Tziperman, E
Zanna, L
Penland, C
Nonnormal thermohaline circulation dynamics in a coupled ocean-atmosphere GCM
author_facet Tziperman, E
Zanna, L
Penland, C
author_sort Tziperman, E
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
publishDate 2016
url https://doi.org/10.1175/2007JPO3769.1
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genre North Atlantic
genre_facet North Atlantic
op_relation doi:10.1175/2007JPO3769.1
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https://doi.org/10.1175/2007JPO3769.1
op_rights info:eu-repo/semantics/embargoedAccess
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
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