Observed amplification of the seasonal CO2 cycle at the Southern Ocean Time Series

被引：7

作者：

Shadwick, Elizabeth H. ^{[1
,2
]}

Wynn-Edwards, Cathryn A. ^{[1
,2
]}

Matear, Richard J. ^{[1
]}

Jansen, Peter ^{[1
]}

Schulz, Eric ^{[3
]}

Sutton, Adrienne J. ^{[4
]}

机构：

[1] Commonwealth Sci & Ind Res Org CSIRO Environm, Hobart, Tas, Australia

[2] Univ Tasmania, Australian Antarctic Program Partnership AAPP, Hobart, Tas, Australia

[3] Bur Meteorol, Melbourne, Vic, Australia

[4] Natl Ocean & Atmospher Adm NOAA, Pacific Marine Environm Lab, Seattle, WA USA

来源：

FRONTIERS IN MARINE SCIENCE | 2023年 / 10卷

关键词：

CO2 partial pressure (pCO(2)); Southern Ocean Time Series (SOTS); pCO(2) seasonality; air-sea CO2 flux; ocean acidification; SEAWATER PCO(2); CARBON-DIOXIDE; INTERANNUAL VARIABILITY; ANTHROPOGENIC CARBON; MIXED-LAYER; WIND-SPEED; TRENDS; FLUX; DRIVERS; SINK;

D O I：

10.3389/fmars.2023.1281854

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

The Subantarctic Zone, the circumpolar region of the Southern Ocean between the Subtropical and Subantarctic fronts, plays an important role in air-sea CO2 exchange, the storage of anthropogenic CO2, and the ventilation of the lower thermocline. Here we use a time series from moored platforms deployed between 2011 and 2021 as part of the Southern Ocean Time Series (SOTS) observatory to investigate the seasonality and interannual variability of upper ocean hydrography and seawater CO2 partial pressure (pCO(2)). The region is a net sink for atmospheric CO2 over the nearly 10-year record, with trends revealing that the ocean pCO(2) may be increasing slightly faster than the atmosphere, suggesting that oceanic as well as anthropogenic atmospheric forcing contributes to the decadal change, which includes a decline in pH on the order of 0.003 yr(-1). The observations also show an amplification of the seasonal cycle in pCO(2), potentially linked to changes in mixed layer depth and biological productivity.

引用

页数：11

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