We estimated mixed layer gross and net community production on a total of 20 crossings in the Australian sector of the Southern Ocean during the summer half-years (October-March) of 2007-2010. These estimates were calculated from measurements of O-2/Ar ratios and triple isotope compositions of O-2 in similar to 250 seawater samples collected underway. For comparison purposes, we also measured the seasonal drawdown of mixed layer NO3- and SiO2 concentrations during 2006-2007 and 2007-2008. Across all samples, average values of gross and net O-2 production (measured by O-2/Ar and O-2 isotopes), were about 86 +/- 90 and 18 +/- 17 mmol O-2 m(-2) day(-1), respectively. Gross production was highest at the Subtropical Front (up to similar to 230 mmol O-2 m(-2) day(-1)), and decreased southward (to similar to 10 near the southern boundary of the Antarctic Circumpolar Current). In contrast, net community production showed little meridional variation. Net and gross O-2 production increased throughout the spring-to-fall period, although most SiO2 drawdown occurred in December. Consistent with satellite chlorophyll estimates, we saw no evidence for an intense spring bloom (e.g. as has been observed in the North Atlantic). Volumetric net and gross O-2 production in the mixed layer, normalized to chlorophyll, increased (with considerable scatter) with average irradiance in the mixed layer. These relationships provide a basis for estimating production from Argo float data and properties observed by satellite. (C) 2016 Elsevier Ltd. All rights reserved.
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Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Science and Technology InnovatKey Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Science and Technology Innovat
Lijuan WANG
Aiguo DAI
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Department of Atmospheric and Environmental Sciences, University at Albany,SUNY
National Center for Atmospheric ResearchKey Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Science and Technology Innovat
Aiguo DAI
Shuaihong GUO
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Meteorological Observatory of No.95147 Unit of PLAKey Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Science and Technology Innovat
Shuaihong GUO
Jing GE
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Key Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Science and Technology InnovatKey Laboratory of Meteorological Disaster, Ministry of Education/Joint International Research Laboratory of Climate and Environment Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Science and Technology Innovat