A Continental Shelf Pump for CO 2 on the Adelie Land Coast, East Antarctica
A Continental Shelf Pump for CO 2 on the Adelie Land Coast, East Antarctica
复制标题
南极洲东部阿德利陆地海岸的 CO 2 大陆架泵
DOI:
10.1029/2020jc016302
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发表时间:
2020
期刊:
影响因子:
--
通讯作者:
Kusahara Kazuya
中科院分区:
文献类型:
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作者:
Arroyo Mar C.;Shadwick Elizabeth H.;Tilbrook Bronte;Rintoul Stephen R.;Kusahara Kazuya
We quantify the transport of inorganic carbon from the continental shelf to the deep ocean in Dense Shelf Water (DSW) from the Mertz and Ninnis Polynyas along the Adélie Land coast in East Antarctica. For this purpose, observations of total dissolved inorganic carbon (TCO2) from two summer hydrographic surveys in 2015 and 2017 were paired with DSW volume transport estimates derived from a coupled ocean‐sea ice‐ice shelf model to examine the fate of inorganic carbon in DSW from Adélie Land. Transports indicate a net outflow of 227 ± 115 Tg C yr−1with DSW in the postglacial calving configuration of the Mertz Polynya. The greatest outflow of inorganic carbon from the shelf region was delivered through the northern boundary across the Adélie and Mertz Sills, with an additional transport westward from the Mertz Polynya. Inorganic carbon in DSW is derived primarily from inflowing TCO2‐rich modified Circumpolar Deep Water; local processes (biological productivity, air‐sea exchange of CO2, and the addition of brine during sea ice formation) make much smaller contributions. This study proposes that DSW export serves as a continental shelf pump for CO2and is a pathway to sequester inorganic carbon from the shallow Antarctic continental shelf to the abyssal ocean, removing CO2from atmospheric exchange on the time scale of centuries.