globalchange  > 气候减缓与适应
DOI: 10.1029/2017JC012917
Scopus记录号: 2-s2.0-85050794402
论文题名:
Assessment of the Carbonate Chemistry Seasonal Cycles in the Southern Ocean From Persistent Observational Platforms
作者: Williams N.L.; Juranek L.W.; Feely R.A.; Russell J.L.; Johnson K.S.; Hales B.
刊名: Journal of Geophysical Research: Oceans
ISSN: 21699275
出版年: 2018
卷: 123, 期:7
起始页码: 4833
结束页码: 4852
语种: 英语
英文关键词: autonomous floats ; climate change ; climatology ; ocean carbon cycle ; pH ; Southern Ocean
英文摘要: Observations from Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) biogeochemical profiling Argo floats are used to characterize the climatological seasonal cycles and drivers of dissolved inorganic carbon, total alkalinity, pH, the partial pressure of carbon dioxide (CO2), and the saturation state of aragonite at the surface and at 200 m across five Southern Ocean frontal regimes, including under sea ice. The Southern Ocean ranges from a temperature-dominated system in the northernmost Subtropical Zone to a biologically dominated system in the most poleward Seasonal Sea Ice Zone. In all zones, the ingassing or outgassing of CO2 must be balanced by geostrophic and Ekman transport, mixing from below, and particle transport of carbon into or out of the euphotic zone. The climatological seasonal cycles spanning the period from 2014 to 2017 compare favorably with existing climatologies in spring and summer and less so during winter months, at higher latitudes, and in ice-covered regions due, in part, to limited wintertime observations before SOCCOM. We observe increases in the carbon and nutrient content of surface waters south of the Subantarctic Front between climatological data products and the SOCCOM float climatologies, even after adjusting for anthropogenic change, suggesting a large-scale increase in the amount of upwelled carbon- and nutrient-rich deep waters. This increased upwelling corresponds to a positive Southern Annular Mode Index over 2014–2017 and likely acts to decrease the magnitude of the Southern Ocean sink of total carbon by increasing outgassing of natural CO2, especially during winter months. ©2018. American Geophysical Union. All Rights Reserved.
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被引频次[WOS]:42   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/113614
Appears in Collections:气候减缓与适应

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作者单位: College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, United States; Pacific Marine Environmental Laboratory, NOAA, Seattle, WA, United States; Pacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, WA, United States; Department of Geosciences, University of Arizona, Tucson, AZ, United States; Monterey Bay Aquarium Research Institute, Moss Landing, CA, United States

Recommended Citation:
Williams N.L.,Juranek L.W.,Feely R.A.,et al. Assessment of the Carbonate Chemistry Seasonal Cycles in the Southern Ocean From Persistent Observational Platforms[J]. Journal of Geophysical Research: Oceans,2018-01-01,123(7)
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