Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments

We analyze the sensitivity of the oceanic thermohaline circulation (THC) regarding perturbations in fresh water flux for a range of coupled oceanic general circulation - atmospheric energy balance models. The energy balance model (EBM) predicts surface air temperature and fresh water flux and contai...

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Main Authors: Lohmann, Gerrit, Gerdes, Rüdiger, Chen, D.
Format: Article in Journal/Newspaper
Language:unknown
Published: 1996
Subjects:
Online Access:https://epic.awi.de/id/eprint/1986/
https://epic.awi.de/id/eprint/1986/1/Loh1996a.pdf
https://hdl.handle.net/10013/epic.12577
https://hdl.handle.net/10013/epic.12577.d001
id ftawi:oai:epic.awi.de:1986
record_format openpolar
spelling ftawi:oai:epic.awi.de:1986 2023-09-05T13:23:30+02:00 Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments Lohmann, Gerrit Gerdes, Rüdiger Chen, D. 1996 application/pdf https://epic.awi.de/id/eprint/1986/ https://epic.awi.de/id/eprint/1986/1/Loh1996a.pdf https://hdl.handle.net/10013/epic.12577 https://hdl.handle.net/10013/epic.12577.d001 unknown https://epic.awi.de/id/eprint/1986/1/Loh1996a.pdf https://hdl.handle.net/10013/epic.12577.d001 Lohmann, G. orcid:0000-0003-2089-733X , Gerdes, R. and Chen, D. (1996) Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments , Climate Dynamics, 12 , pp. 403-416 . hdl:10013/epic.12577 EPIC3Climate Dynamics, 12, pp. 403-416 Article isiRev 1996 ftawi 2023-08-22T19:43:00Z We analyze the sensitivity of the oceanic thermohaline circulation (THC) regarding perturbations in fresh water flux for a range of coupled oceanic general circulation - atmospheric energy balance models. The energy balance model (EBM) predicts surface air temperature and fresh water flux and contains the feedbacks due to meridional transports of sensible and latent heat. In the coupled system we examine a negative perturbation in run-off into the southern ocean and analyze the role of changed atmospheric heat transports and fresh water flux. With mixed boundary conditions (fixed air temperature and fixed surface fresh water fluxes) the response is characterised by a completely different oceanic heat transport than in the reference case. On the other hand, the surface heat flux remains roughly constant when the air temperature can adjust in a model where no anomalous atmospheric transports are allowed. This gives an artificially stable system with nearly unchanged oceanic heat transport. However, if meridional heat transports in the atmosphere are included, the sensitivity of the system lies between the two extreme cases. We find that changes in fresh water flux are unimportant for the THC in the coupled system. Article in Journal/Newspaper Southern Ocean Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Southern Ocean
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description We analyze the sensitivity of the oceanic thermohaline circulation (THC) regarding perturbations in fresh water flux for a range of coupled oceanic general circulation - atmospheric energy balance models. The energy balance model (EBM) predicts surface air temperature and fresh water flux and contains the feedbacks due to meridional transports of sensible and latent heat. In the coupled system we examine a negative perturbation in run-off into the southern ocean and analyze the role of changed atmospheric heat transports and fresh water flux. With mixed boundary conditions (fixed air temperature and fixed surface fresh water fluxes) the response is characterised by a completely different oceanic heat transport than in the reference case. On the other hand, the surface heat flux remains roughly constant when the air temperature can adjust in a model where no anomalous atmospheric transports are allowed. This gives an artificially stable system with nearly unchanged oceanic heat transport. However, if meridional heat transports in the atmosphere are included, the sensitivity of the system lies between the two extreme cases. We find that changes in fresh water flux are unimportant for the THC in the coupled system.
format Article in Journal/Newspaper
author Lohmann, Gerrit
Gerdes, Rüdiger
Chen, D.
spellingShingle Lohmann, Gerrit
Gerdes, Rüdiger
Chen, D.
Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments
author_facet Lohmann, Gerrit
Gerdes, Rüdiger
Chen, D.
author_sort Lohmann, Gerrit
title Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments
title_short Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments
title_full Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments
title_fullStr Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments
title_full_unstemmed Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments
title_sort sensitivity of the thermohaline circulation in coupled oceanic gcm - atmospheric ebm experiments
publishDate 1996
url https://epic.awi.de/id/eprint/1986/
https://epic.awi.de/id/eprint/1986/1/Loh1996a.pdf
https://hdl.handle.net/10013/epic.12577
https://hdl.handle.net/10013/epic.12577.d001
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source EPIC3Climate Dynamics, 12, pp. 403-416
op_relation https://epic.awi.de/id/eprint/1986/1/Loh1996a.pdf
https://hdl.handle.net/10013/epic.12577.d001
Lohmann, G. orcid:0000-0003-2089-733X , Gerdes, R. and Chen, D. (1996) Sensitivity of the thermohaline circulation in coupled oceanic GCM - atmospheric EBM experiments , Climate Dynamics, 12 , pp. 403-416 . hdl:10013/epic.12577
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