FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1982300900> ?p ?o ?g. }

• W1982300900 endingPage "n/a" @default.
• W1982300900 startingPage "n/a" @default.
• W1982300900 abstract "One potential mechanism for lowering atmospheric CO2 during glacial times is an increase in the fraction of the global ocean ventilated by the North Atlantic, which produces deep water with a low concentration of unused nutrients and thus drives the ocean's biological pump to a high efficiency. However, the data indicate that during glacial times, a water mass low in 13C/12C and 14C/C occupied the deep Atlantic, apparently at the expense of North Atlantic Deep Water (NADW). This water is commonly referred to as “southern-sourced” because of its apparent entry into the Atlantic basin from the South, prompting the inference that it was ventilated at the Southern Ocean surface. Here, we propose that this deep Atlantic water mass actually included a large fraction of North Atlantic-ventilated water, the chemical characteristics of which were altered by recirculation in the deep Southern and Indo-Pacific oceans. In an ocean model sensitivity experiment that reduces Antarctic Bottom Water formation and weakens its overturning circulation, we find that a much greater fraction of NADW is transported into the Southern Ocean without contacting the surface and is entrained and mixed into the southern-sourced deep water that spreads into the global abyssal ocean. Thus, North Atlantic ventilation takes over more of the ocean interior, lowering atmospheric CO2, and yet the abyssal Atlantic is filled from the South with old water low in 13C/12C and 14C/C, consistent with glacial data." @default.
• W1982300900 created "2016-06-24" @default.
• W1982300900 creator A5013009757 @default.
• W1982300900 creator A5019280918 @default.
• W1982300900 creator A5027305185 @default.
• W1982300900 creator A5041012419 @default.
• W1982300900 creator A5055080953 @default.
• W1982300900 creator A5056786516 @default.
• W1982300900 date "2012-05-23" @default.
• W1982300900 modified "2023-10-18" @default.
• W1982300900 title "North Atlantic ventilation of “southern-sourced” deep water in the glacial ocean" @default.
• W1982300900 cites W1489917183 @default.
• W1982300900 cites W1493417715 @default.
• W1982300900 cites W1566807995 @default.
• W1982300900 cites W1594282911 @default.
• W1982300900 cites W1611443029 @default.
• W1982300900 cites W1620458047 @default.
• W1982300900 cites W1644214006 @default.
• W1982300900 cites W1657772896 @default.
• W1982300900 cites W1664033179 @default.
• W1982300900 cites W1677073775 @default.
• W1982300900 cites W1794096300 @default.
• W1982300900 cites W1837986572 @default.
• W1982300900 cites W1963549306 @default.
• W1982300900 cites W1964547159 @default.
• W1982300900 cites W1964806567 @default.
• W1982300900 cites W1965509371 @default.
• W1982300900 cites W1969509303 @default.
• W1982300900 cites W1978064540 @default.
• W1982300900 cites W1978483496 @default.
• W1982300900 cites W1979257792 @default.
• W1982300900 cites W1980799929 @default.
• W1982300900 cites W1986081344 @default.
• W1982300900 cites W1988124533 @default.
• W1982300900 cites W1990753866 @default.
• W1982300900 cites W1992971439 @default.
• W1982300900 cites W1997001246 @default.
• W1982300900 cites W2000766006 @default.
• W1982300900 cites W2011374672 @default.
• W1982300900 cites W2012434986 @default.
• W1982300900 cites W2013380149 @default.
• W1982300900 cites W2014727327 @default.
• W1982300900 cites W2018156694 @default.
• W1982300900 cites W2018424764 @default.
• W1982300900 cites W2018434487 @default.
• W1982300900 cites W2018799022 @default.
• W1982300900 cites W2028443916 @default.
• W1982300900 cites W2030098873 @default.
• W1982300900 cites W2035800339 @default.
• W1982300900 cites W2035919032 @default.
• W1982300900 cites W2042125781 @default.
• W1982300900 cites W2042189564 @default.
• W1982300900 cites W2042476750 @default.
• W1982300900 cites W2045998803 @default.
• W1982300900 cites W2047623512 @default.
• W1982300900 cites W2048583402 @default.
• W1982300900 cites W2048862519 @default.
• W1982300900 cites W2049429560 @default.
• W1982300900 cites W2051226623 @default.
• W1982300900 cites W2051246904 @default.
• W1982300900 cites W2057377643 @default.
• W1982300900 cites W2060812013 @default.
• W1982300900 cites W2060839089 @default.
• W1982300900 cites W2062800482 @default.
• W1982300900 cites W2063176407 @default.
• W1982300900 cites W2064368240 @default.
• W1982300900 cites W2067150205 @default.
• W1982300900 cites W2067277521 @default.
• W1982300900 cites W2074901826 @default.
• W1982300900 cites W2090767277 @default.
• W1982300900 cites W2091771644 @default.
• W1982300900 cites W2106441671 @default.
• W1982300900 cites W2111653154 @default.
• W1982300900 cites W2112428814 @default.
• W1982300900 cites W2114462220 @default.
• W1982300900 cites W2117011490 @default.
• W1982300900 cites W2119989333 @default.
• W1982300900 cites W2120651032 @default.
• W1982300900 cites W2124083617 @default.
• W1982300900 cites W2126730472 @default.
• W1982300900 cites W2129542530 @default.
• W1982300900 cites W2135465384 @default.
• W1982300900 cites W2135476338 @default.
• W1982300900 cites W2146493061 @default.
• W1982300900 cites W2149769204 @default.
• W1982300900 cites W2155435132 @default.
• W1982300900 cites W2161480748 @default.
• W1982300900 cites W2168812594 @default.
• W1982300900 cites W2170698755 @default.
• W1982300900 cites W2171106889 @default.
• W1982300900 cites W3023105105 @default.
• W1982300900 cites W4211135859 @default.
• W1982300900 cites W4255263969 @default.
• W1982300900 cites W4294555410 @default.
• W1982300900 doi "https://doi.org/10.1029/2011pa002211" @default.
• W1982300900 hasPublicationYear "2012" @default.
• W1982300900 type Work @default.
• W1982300900 sameAs 1982300900 @default.

• next