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Influence of the oceanic biology on the tropical Pacific climate in a coupled general circulation model

Influence of the oceanic biology on the tropical Pacific climate in a coupled general circulation model
Influence of the oceanic biology on the tropical Pacific climate in a coupled general circulation model
The influence of chlorophyll spatial patterns and variability on the tropical Pacific climate is investigated by using a fully coupled general circulation model (HadOPA) coupled to a state-of-the-art biogeochemical model (PISCES). The simulated chlorophyll concentrations can feedback onto the ocean by modifying the vertical distribution of radiant heating. This fully interactive biological-ocean-atmosphere experiment is compared to a reference experiment that uses a constant chlorophyll concentration (0.06 mg m?3). It is shown that introducing an interactive biology acts to warm the surface eastern equatorial Pacific by about 0.5°C. Two competing processes are involved in generating this warming: (a) a direct 1-D biological warming process in the top layers (0–30 m) resulting from strong chlorophyll concentrations in the upwelling region and enhanced by positive dynamical feedbacks (weaker trade winds, surface currents and upwelling) and (b) a 2-D meridional cooling process which brings cold off-equatorial anomalies from the subsurface into the equatorial mixed layer through the meridional cells. Sensitivity experiments show that the climatological horizontal structure of the chlorophyll field in the upper layers is crucial to maintain the eastern Pacific warming. Concerning the variability, introducing an interactive biology slightly reduces the strength of the seasonal cycle, with stronger SST warming and chlorophyll concentrations during the upwelling season. In addition, ENSO amplitude is slightly increased. Similar experiments performed with another coupled general circulation model (IPSL-CM4) exhibit the same behaviour as in HadOPA, hence showing the robustness of the results.
0930-7575
503-516
Lengaigne, Matthieu
3f78eafe-bcd2-41c4-9e0e-3b8bb3c55aa4
Menkes, Christophe
5471b65b-0584-49ff-b27f-4c7b29e75bbd
Aumont, Olivier
6ea5af9d-4c27-42d9-9ba7-749729efa72f
Gorgues, Thomas
a8138c6c-bd72-4c65-a974-76bad8b88b70
Bopp, Laurent
771de655-3caf-42ba-8231-40f17d4addc4
André, Jean-Michel
a7522186-9f15-41bd-9509-6730f6e7e532
Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864
Lengaigne, Matthieu
3f78eafe-bcd2-41c4-9e0e-3b8bb3c55aa4
Menkes, Christophe
5471b65b-0584-49ff-b27f-4c7b29e75bbd
Aumont, Olivier
6ea5af9d-4c27-42d9-9ba7-749729efa72f
Gorgues, Thomas
a8138c6c-bd72-4c65-a974-76bad8b88b70
Bopp, Laurent
771de655-3caf-42ba-8231-40f17d4addc4
André, Jean-Michel
a7522186-9f15-41bd-9509-6730f6e7e532
Madec, Gurvan
ffb28deb-4bbd-4a4c-914f-492f813e4864

Lengaigne, Matthieu, Menkes, Christophe, Aumont, Olivier, Gorgues, Thomas, Bopp, Laurent, André, Jean-Michel and Madec, Gurvan (2007) Influence of the oceanic biology on the tropical Pacific climate in a coupled general circulation model. Climate Dynamics, 28 (5), 503-516. (doi:10.1007/s00382-006-0200-2).

Record type: Article

Abstract

The influence of chlorophyll spatial patterns and variability on the tropical Pacific climate is investigated by using a fully coupled general circulation model (HadOPA) coupled to a state-of-the-art biogeochemical model (PISCES). The simulated chlorophyll concentrations can feedback onto the ocean by modifying the vertical distribution of radiant heating. This fully interactive biological-ocean-atmosphere experiment is compared to a reference experiment that uses a constant chlorophyll concentration (0.06 mg m?3). It is shown that introducing an interactive biology acts to warm the surface eastern equatorial Pacific by about 0.5°C. Two competing processes are involved in generating this warming: (a) a direct 1-D biological warming process in the top layers (0–30 m) resulting from strong chlorophyll concentrations in the upwelling region and enhanced by positive dynamical feedbacks (weaker trade winds, surface currents and upwelling) and (b) a 2-D meridional cooling process which brings cold off-equatorial anomalies from the subsurface into the equatorial mixed layer through the meridional cells. Sensitivity experiments show that the climatological horizontal structure of the chlorophyll field in the upper layers is crucial to maintain the eastern Pacific warming. Concerning the variability, introducing an interactive biology slightly reduces the strength of the seasonal cycle, with stronger SST warming and chlorophyll concentrations during the upwelling season. In addition, ENSO amplitude is slightly increased. Similar experiments performed with another coupled general circulation model (IPSL-CM4) exhibit the same behaviour as in HadOPA, hence showing the robustness of the results.

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Published date: 28 April 2007

Identifiers

Local EPrints ID: 64345
URI: http://eprints.soton.ac.uk/id/eprint/64345
ISSN: 0930-7575
PURE UUID: 1040de81-d3cd-4c36-b8de-4c7e2da56e42

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Date deposited: 10 Dec 2008
Last modified: 15 Mar 2024 11:48

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Contributors

Author: Matthieu Lengaigne
Author: Christophe Menkes
Author: Olivier Aumont
Author: Thomas Gorgues
Author: Laurent Bopp
Author: Jean-Michel André
Author: Gurvan Madec

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