de.mpg.escidoc.pubman.appbase.FacesBean
English
 
Help Guide Disclaimer Contact us Login
  Advanced SearchBrowse

Item

ITEM ACTIONSEXPORT

Released

Journal Article

Bio-optical feedbacks among phytoplankton, upper ocean physics and sea-ice in a global model

MPS-Authors
http://pubman.mpdl.mpg.de/cone/persons/resource/persons62473

Manizza,  M.
Department Biogeochemical Synthesis, Prof. C. Prentice, Max Planck Institute for Biogeochemistry, Max Planck Society;

http://pubman.mpdl.mpg.de/cone/persons/resource/persons62461

Le Quéré,  C.
Department Biogeochemical Synthesis, Prof. C. Prentice, Max Planck Institute for Biogeochemistry, Max Planck Society;

http://pubman.mpdl.mpg.de/cone/persons/resource/persons62351

Buitenhuis,  E. T.
Department Biogeochemical Synthesis, Prof. C. Prentice, Max Planck Institute for Biogeochemistry, Max Planck Society;

Locator
Fulltext (public)
There are no public fulltexts available
Supplementary Material (public)
There is no public supplementary material available
Citation

Manizza, M., Le Quéré, C., Watson, A. J., & Buitenhuis, E. T. (2005). Bio-optical feedbacks among phytoplankton, upper ocean physics and sea-ice in a global model. Geophysical Research Letters, 32(5), L05603. doi:10.1029/2004GL020778.


Cite as: http://hdl.handle.net/11858/00-001M-0000-000E-D328-C
Abstract
Phytoplankton biomass modifies the penetration of light and impacts the physical properties of the upper ocean. We quantify these impacts and the feedbacks on phytoplankton biomass for the global ocean using an Ocean General Circulation Model coupled to an ocean biogeochemistry model. Phytoplankton biomass amplifies the seasonal cycle of temperature, mixed layer depth and ice cover by roughly 10%. At mid and high latitudes, surface temperature warms by 0.1 - 1.5 degrees C in spring/ summer and cools by 0.1 - 0.3 degrees C in fall/ winter. In the tropics, phytoplankton biomass indirectly cools the ocean surface by 0.3 degrees C due to enhanced upwelling. The mixed layer stratifies by 4 - 30 m everywhere except at high latitudes. At high latitudes, the sea- ice cover is reduced by up to 6% in summer and increased by 2% in winter, leading to further feedbacks on vertical mixing and heat fluxes. Physical changes drive a positive feedback increasing phytoplankton biomass by 4 - 12% and further amplifies the initial physical perturbations. [References: 23]