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MODELLING THE FEEDBACKS BETWEEN PHYTOPLANKTON AND GLOBAL OCEAN PHYSICS 1 Max-Planck-Institut für Biogeochemie, Jena, Germany. 2 University of East Anglia, Norwich, United Kingdom. Manfredi Manizza 1,2 , C. Le Quéré 1 , A. J. Watson 2 , E. Buitenhuis 1

MODELLING THE FEEDBACKS BETWEEN PHYTOPLANKTON AND GLOBAL OCEAN PHYSICS

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MODELLING THE FEEDBACKS BETWEEN PHYTOPLANKTON AND GLOBAL OCEAN PHYSICS. Manfredi Manizza 1,2 , C. Le Qu é r é 1 , A. J. Watson 2 , E. Buitenhuis 1. 1 Max-Planck-Institut f ü r Biogeochemie, Jena, Germany. 2 University of East Anglia, Norwich, United Kingdom. Sun. I o. Ocean Surface. - PowerPoint PPT Presentation

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  • MODELLING THE FEEDBACKS BETWEEN PHYTOPLANKTON AND GLOBAL OCEAN PHYSICS 1Max-Planck-Institut fr Biogeochemie, Jena, Germany.2University of East Anglia, Norwich, United Kingdom.Manfredi Manizza1,2, C. Le Qur 1, A. J. Watson2,E. Buitenhuis1

  • PHYTOPLANKTON-LIGHT-HEAT INTERACTION

  • FROM TROPICAL TO GLOBAL 1) An OGCM (OPA) on global configuration: 0.5 - 1.5 x 2.0 (Lat x Lon) 1.5 order TKE Model. Gent-McWilliams eddy-mixing.2) An ocean biogeochemistry model (Dynamic Green Ocean Model) : Diatoms and Coccolithophores and Nanophytoplankton. Micro and Mesozooplankton. Co-limitation of light,P, Si and Fe.3) A Sea-Ice model (LIM) Tropical Studies: Nakamoto et al. (2000, 2001); Murtugudde et al. (2002) OGCM + Satellite derived Chlorophyll Off-line forcing NO FEEDBACKS !!Ocean Surface

  • INCLUDING THE BIOLOGYK() = LIGHT EXTINCTION COEFFICIENTREDBLUE/GREENINFRAREDPaulson & Simpson Model (JPO,1977)Morel Model (JGR,1988)[Chl]tot = [Chl]diatom + [Chl]cocco + [Chl]nano

  • Monthly MaximumTHE MODELLED BIO-FORCING (mg m-3)Monthly AverageSURFACE [Chl]

  • PENETRATION DEPTH (Zpen)IoZpenZpen = (ez I (z) dz)/Io Average(m)Zpen Visible Light = 23 m

  • TROPICS

  • Average SEA SURFACE TEMPERATURE C TEMPERATURE C

  • MLD & u(surf)Average(m)

  • TROPICS TO SUB-TROPICS

  • TROPICS/SUBTROPICS INTERACTION EquatorSubtropicsSubtropics+PO4-MLD+u+TPP

    TOTALPRIMARYPRODUCTIONgC m-2 yr-1

    MONTHLY AVERAGE DEPTH

  • HIGH LATITUDES

  • SEA SURFACE TEMPERATURE Monthly Maximum C

  • EFFECTS ON SEA-ICE (AVERAGE) %ICEN = -0.17 * [Chl]surf %ICES = -1.3 * [Chl]surf%(Ice fraction)Sea-iceOceanSunPhytoplankton

  • GLOBAL

  • ECOSYSTEM RESPONSE Total Chl (mg m-3)Diatoms (%)Coccolithophores (%)Nanophyto (%) AVERAGE

  • IMPACT ON OCEAN CARBON CYCLE

  • CONCLUSIONS Different and Regional Modifications: SST, MLD, CURRENTS, SEA-ICE. OCEAN PHYSICS ECOSYSTEM & OCEAN BIOGEOCHEMISTRY OCEAN CARBON CYCLE. Global OBGCM Tropics and Interaction Tropics/Subtropics & High Latitudes. Phytoplankton presence affects light and heat penetration in the ocean.

  • Dynamic Green Ocean Model(Buitenhuis et al.,in prep.)

    In the Community Land Model, vegetation is not represented as biomes (e.g., savanna) but rather as patches of plant functional types (e.g., grasses, trees).