Spatial and temporal variability of biogenic gases during the Southern Ocean spring bloom

被引:32
|
作者
Tortell, Philippe D. [1 ,2 ]
Long, Matthew C. [3 ]
机构
[1] Univ British Columbia, Dept Earth & Ocean Sci, Vancouver, BC V6T 1Z4, Canada
[2] Univ British Columbia, Dept Bot, Vancouver, BC V6T 1Z4, Canada
[3] Stanford Univ, Dept Environm Earth Syst Sci, Stanford, CA 94305 USA
基金
加拿大自然科学与工程研究理事会;
关键词
SEA-ICE; DIMETHYLSULFIDE DMS; CARBON-DIOXIDE; NEW-ZEALAND; CO2; FLUX; CLIMATE; WATERS; IRON; PHYTOPLANKTON; O-2/AR;
D O I
10.1029/2008GL035819
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Southern Ocean exerts a strong influence on global biogeochemical cycles and air-sea gas fluxes. Significant progress has been made towards understanding the general patterns of circulation and biological productivity in this region, but the small-scale dynamics of surface water gases remain poorly resolved. Here we present new data documenting unprecedented spatial and temporal variability of Southern Ocean biogenic gases during the spring phytoplankton bloom. Using real-time underway mass spectrometry, we observed significant changes in surface water O(2)/Ar, pCO(2), and dimethylsulfide (DMS) concentrations over time scales of days to weeks and sub-km spatial scales. Our results demonstrate a tight coupling between physical and biological processes controlling Southern Ocean gas distributions, and highlight the distinct biogeochemical dynamics governing gas cycling in open water and ice-covered regions. Citation: Tortell, P. D., and M. C. Long ( 2009), Spatial and temporal variability of biogenic gases during the Southern Ocean spring bloom, Geophys. Res. Lett., 36, L01603, doi: 10.1029/2008GL035819.
引用
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页数:5
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