Ecosystem dynamics based on plankton functional types for global ocean biogeochemistry models

被引:645
作者
Le Quéré, C
Harrison, SP
Prentice, IC
Buitenhuis, ET
Aumont, O
Bopp, L
Claustre, H
Da Cunha, LC
Geider, R
Giraud, X
Klaas, C
Kohfeld, KE
Legendre, L
Manizza, M
Platt, T
Rivkin, RB
Sathyendranath, S
Uitz, J
Watson, AJ
Wolf-Gladrow, D
机构
[1] Univ E Anglia, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England
[2] Max Planck Inst Biogeochem, D-07701 Jena, Germany
[3] Univ Bristol, Sch Geog Sci, Bristol BS8 1SS, Avon, England
[4] Univ Bristol, Dept Earth Sci, QUEST, Bristol BS8 1RJ, Avon, England
[5] Univ Paris 06, Lab Oceanog Dynam & Climat, F-75005 Paris, France
[6] Lab Sci Climat & Environm, F-91191 Gif Sur Yvette, France
[7] Lab Oceanog Villefranche, F-06238 Villefranche Sur Mer, France
[8] Univ Essex, Dept Sci Biol, Colchester CO4 3SQ, Essex, England
[9] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany
[10] Dalhousie Univ, Dept Oceanog, Halifax, NS B3H 4J1, Canada
[11] Mem Univ Newfoundland, Ctr Ocean Sci, St John, NF A1C 5S7, Canada
基金
英国自然环境研究理事会;
关键词
carbon cycle; climate change; ecosystem; functional types; glacial-interglacial cycles; modeling; ocean; plankton;
D O I
10.1111/j.1365-2468.2005.01004.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Ecosystem processes are important determinants of the biogeochemistry of the ocean, and they can be profoundly affected by changes in climate. Ocean models currently express ecosystem processes through empirically derived parameterizations that tightly link key geochemical tracers to ocean physics. The explicit inclusion of ecosystem processes in models will permit ecological changes to be taken into account, and will allow us to address several important questions, including the causes of observed glacial-interglacial changes in atmospheric trace gases and aerosols, and how the oceanic uptake of CO2 is likely to change in the future. There is an urgent need to assess our mechanistic understanding of the environmental factors that exert control over marine ecosystems, and to represent their natural complexity based on theoretical understanding. We present a prototype design for a Dynamic Green Ocean Model (DGOM) based on the identification of (a) key plankton functional types that need to be simulated explicitly to capture important biogeochemical processes in the ocean; (b) key processes controlling the growth and mortality of these functional types and hence their interactions; and (c) sources of information necessary to parameterize each of these processes within a modeling framework. We also develop a strategy for model evaluation, based on simulation of both past and present mean state and variability, and identify potential sources of validation data for each. Finally, we present a DGOM-based strategy for addressing key questions in ocean biogeochemistry. This paper thus presents ongoing work in ocean biogeochemical modeling, which, it is hoped will motivate international collaborations to improve our understanding of the role of the ocean in the climate system.
引用
收藏
页码:2016 / 2040
页数:25
相关论文
共 191 条
[1]  
ALVAIN S, 2005, IN PRESS DEEP SEA RE
[2]   Spatial and temporal variability of particle flux at the NW European continental margin [J].
Antia, AN ;
Maassen, J ;
Herman, P ;
Voss, M ;
Scholten, J ;
Groom, S ;
Miller, P .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2001, 48 (14-15) :3083-3106
[3]   A Model of the iron cycle in the ocean [J].
Archer, DE ;
Johnson, K .
GLOBAL BIOGEOCHEMICAL CYCLES, 2000, 14 (01) :269-279
[4]   Transformation of dimethylsulphoniopropionate to dimethyl sulphide during summer in the North Sea with an examination of key processes via a modelling approach [J].
Archer, SD ;
Gilbert, FJ ;
Nightingale, PD ;
Zubkov, MV ;
Taylor, AH ;
Smith, GC ;
Burkill, PH .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2002, 49 (15) :3067-3101
[5]  
Armstrong RA, 2003, MODELS IN ECOSYSTEM SCIENCE, P254
[6]   A hybrid spectral representation of phytoplankton growth and zooplankton response: The "control rod" model of plankton interaction [J].
Armstrong, RA .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2003, 50 (22-26) :2895-2916
[7]   An ecosystem model of the global ocean including Fe, Si, P colimitations [J].
Aumont, O ;
Maier-Reimer, E ;
Blain, S ;
Monfray, P .
GLOBAL BIOGEOCHEMICAL CYCLES, 2003, 17 (02)
[8]   Dimethylsulfoniopropionate (DMSP) and dimethylsulfide (DMS) sea surface distributions simulated from a global three-dimensional ocean carbon cycle model [J].
Aumont, O ;
Belviso, S ;
Monfray, P .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2002, 107 (C4)
[9]   RATES OF PHYTOPLANKTON CELL-DIVISION IN THE FIELD AND IN IRON ENRICHMENT EXPERIMENTS [J].
BANSE, K .
LIMNOLOGY AND OCEANOGRAPHY, 1991, 36 (08) :1886-1898
[10]   THE EUROPEAN-REGIONAL-SEAS-ECOSYSTEM-MODEL, A COMPLEX MARINE ECOSYSTEM MODEL [J].
BARETTA, JW ;
EBENHOH, W ;
RUARDIJ, P .
NETHERLANDS JOURNAL OF SEA RESEARCH, 1995, 33 (3-4) :233-246