Southern Ocean Biogeochemical Float Deployment Strategy, With Example From the Greenwich Meridian Line (GO‐SHIP A12)
Southern Ocean Biogeochemical Float Deployment Strategy, With Example From the Greenwich Meridian Line (GO‐SHIP A12)
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南大洋生物地球化学浮标部署策略,以格林威治子午线为例 (GO-SHIP A12)
DOI:
10.1029/2018jc014059
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发表时间:
2019
期刊:
影响因子:
--
通讯作者:
J. Sarmiento
中科院分区:
文献类型:
--
作者:
L. Talley;I. Rosso;I. Kamenkovich;M. Mazloff;J. Wang;E. Boss;A. Gray;K. Johnson;R. Key;S. Riser;N. Williams;J. Sarmiento
Abstract Biogeochemical Argo floats, profiling to 2,000‐m depth, are being deployed throughout the Southern Ocean by the Southern Ocean Carbon and Climate Observations and Modeling program (SOCCOM). The goal is 200 floats by 2020, to provide the first full set of annual cycles of carbon, oxygen, nitrate, and optical properties across multiple oceanographic regimes. Building from no prior coverage to a sparse array, deployments are based on prior knowledge of water mass properties, mean frontal locations, mean circulation and eddy variability, winds, air‐sea heat/freshwater/carbon exchange, prior Argo trajectories, and float simulations in the Southern Ocean State Estimate and Hybrid Coordinate Ocean Model (HYCOM). Twelve floats deployed from the 2014–2015 Polarstern cruise from South Africa to Antarctica are used as a test case to evaluate the deployment strategy adopted for SOCCOM's 20 deployment cruises and 126 floats to date. After several years, these floats continue to represent the deployment zones targeted in advance: (1) Weddell Gyre sea ice zone, observing the Antarctic Slope Front, and a decadally‐rare polynya over Maud Rise; (2) Antarctic Circumpolar Current (ACC) including the topographically steered Southern Zone chimney where upwelling carbon/nutrient‐rich deep waters produce surprisingly large carbon dioxide outgassing; (3) Subantarctic and Subtropical zones between the ACC and Africa; and (4) Cape Basin. Argo floats and eddy‐resolving HYCOM simulations were the best predictors of individual SOCCOM float pathways, with uncertainty after 2 years of order 1,000 km in the sea ice zone and more than double that in and north of the ACC.
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影响因子:
3.5
作者:
A. Thompson;J. Sallée
通讯作者:
A. Thompson;J. Sallée
影响因子:
3.5
作者:
A. Thompson;A. N. Garabato
通讯作者:
A. Thompson;A. N. Garabato
DOI:
10.1029/2017jc012990
发表时间:
2018
期刊:
Journal of Geophysical Research: Oceans
影响因子:
--
作者:
Chamberlain, Paul M.;Talley, Lynne D.;Mazloff, Matthew R.;Riser, Stephen C.;Speer, Kevin;Gray, Alison R.;Schwartzman, Armin
通讯作者:
Schwartzman, Armin
影响因子:
2.2
作者:
Wang, Tianyu;Gille, Sarah T.;Mazloff, Matthew R.;Zilberman, Nathalie V.;Du, Yan
通讯作者:
Du, Yan
影响因子:
3.6
作者:
Russell, Joellen L.;Kamenkovich, Igor;Wanninkhof, Rik
通讯作者:
Wanninkhof, Rik