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Spatial and temporal variability and size fractionation of chlorophyll a in the tropical and subtropical Pacific Ocean

Spatial and temporal variability and size fractionation of chlorophyll a in the tropical and subtropical Pacific Ocean

作     者:ZHANG Dongsheng WANG Chunsheng LIU Zhensheng XU Xuewei WANG Xiaogu ZHOU Yadong 

作者机构:Laboratory of Marine Ecosystem and BiogeochemistryState Oceanic AdministrationHangzhou 310012China 

出 版 物:《Acta Oceanologica Sinica》 (海洋学报(英文版))

年 卷 期:2012年第31卷第3期

页      面:120-131页

核心收录:

学科分类:07[理学] 

基  金:The Scientific Research Fund of the Second Institute of Oceanography,SOA under contract No. JG1024 the COMRA Special Foundation under contract Nos DY125-13-E-01 and DY125-14-E-02 

主  题:chlorophyll a size fractionation Pacific Ocean 

摘      要:The spatial and temporal variability and size fractionation of chlorophyll a (Chl a) were investigated in the tropical and subtropical Pacific Ocean during four survey cruises from 2005 to *** surface Chl a (S-Chl a) concentration ranged from 0.002 to 0.497 mg/m3 and was obviously higher in the eastern Pacific than in the western and central *** vertical distribution of Chl a displayed a single peak pattern,and the maximum Chl a layer (MCL) was observed at a shallower depth in the eastern Pacific than in the western *** three size fractions of Chl a measurements in the surface water showed a similar distribution to total Chl a and were found in higher concentrations in the eastern Pacific than in the western and central *** dominated the phytoplankton in the surveyed tropical and subtropical Pacific ***,pico-Chl a (0.2-2 μm) accounted for a larger percentage of the total Chl a in the central Pacific than it did in the western Pacific and eastern *** the western Pacific,there seemed to be a latitudinal variability in the phytoplankton community composition where small-sized phytoplankton (2 μm) were more dominant in the tropical than in the subtropical western *** spatial and temporal variability and size fractionation of Chl a were controlled by hydrological and chemical characteristics and climate events,such as El Ni(n)o and La Ni(n)a.

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