The influence of the Indian Ocean Dipole on interannual variations in phytoplankton size structure as revealed by Earth Observation

被引:78
作者
Brewin, Robert J. W. [1 ,2 ,3 ]
Hirata, Takafumi [4 ]
Hardman-Mountford, Nick J. [1 ,2 ]
Lavender, Samantha J. [3 ,5 ]
Sathyendranath, Shubha [1 ]
Barlow, Ray [6 ,7 ]
机构
[1] Plymouth Marine Lab, Plymouth PL1 3DH, Devon, England
[2] PML, Natl Ctr Earth Observat, Plymouth PL1 3DH, Devon, England
[3] Univ Plymouth, Sch Marine Sci & Engn, Plymouth PL4 8AA, Devon, England
[4] Hokkaido Univ, Fac Environm Earth Sci, Kita Ku, Sapporo, Hokkaido 0600810, Japan
[5] ARGANS Ltd, Unit 3, Plymouth PL6 8BY, Devon, England
[6] Bayworld Ctr Res & Educ, ZA-8012 Cape Town, South Africa
[7] Univ Cape Town, Marine Res Inst, ZA-7701 Rondebosch, South Africa
基金
美国国家航空航天局;
关键词
Indian Ocean; Phytoplankton; Size; Interannual; Ocean colour; Remote sensing; Chlorophyll-a; SeaWiFS; COMMUNITY STRUCTURE; EQUATORIAL PACIFIC; FUNCTIONAL TYPES; CLIMATE-CHANGE; CHLOROPHYLL-A; ARABIAN SEA; COLOR; VARIABILITY; ABSORPTION; TEMPERATURE;
D O I
10.1016/j.dsr2.2012.04.009
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Using a decade of satellite ocean-colour observations and a model that links chlorophyll-a to the size of the phytoplankton cells, parameterised using pigment data from the Indian Ocean, we examine the implications of the Indian Ocean Dipole (IOD) for phytoplankton size structure. The inferred interannual anomalies in phytoplankton size structure are related to those in sea-surface temperature (SST) and sea-surface height (SSH), derived using satellite radiometry and altimetry, and stratification, derived using the Simple Ocean Data Assimilation (SODA) database. In regions influenced by the Indian Ocean Dipole, we observe a tight correlation between phytoplankton size structure and the physical variables, such that interannual variations in the physical variables accounts for up to 70% of the total variance in phytoplankton size structure. For much of the Indian Ocean, low temperature. low SSH and low stratification (indicative of a turbulent environment) are correlated with larger size classes, consistent with theories on coupling between physical-chemical processes and ecosystem structure. To the extent that phytoplankton function is related to its size structure, changes in physical forcing are likely to influence biogeochemical cycles in the region and the pelagic food web. The limitations of our approach are discussed and we highlight future challenges in satellite ocean-colour monitoring, should climate change lead to any modification in our marine ecosystem. (c) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:117 / 127
页数:11
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