Matches in SemOpenAlex for { <https://semopenalex.org/work/W2506463670> ?p ?o ?g. }
- W2506463670 endingPage "8599" @default.
- W2506463670 startingPage "8590" @default.
- W2506463670 abstract "Deepwater circulation plays a central role in global climate. Compared with the Atlantic, the Pacific deepwater circulation's history remains unclear. The Luzon overflow, a branch of the North Pacific deep water, determines the ventilation rate of the South China Sea (SCS) basin. Sedimentary magnetic properties in the SCS reflect millennial-scale fluctuations in deep current intensity and orientation. The data suggest a slightly stronger current at the Last Glacial Maximum compared to the Holocene. But, the most striking increase in deep current occurred during Heinrich stadial 1 (H1) and to a lesser extent during the Younger Dryas (YD). Results of a transient deglacial experiment suggest that the northeastern current strengthening at the entrance of the SCS during H1 and the YD, times of weak North Atlantic Deep Water formation, could be linked to enhanced formation of North Pacific Deep Water." @default.
- W2506463670 created "2016-08-23" @default.
- W2506463670 creator A5000033732 @default.
- W2506463670 creator A5004586541 @default.
- W2506463670 creator A5014186251 @default.
- W2506463670 creator A5024507723 @default.
- W2506463670 creator A5024878311 @default.
- W2506463670 creator A5027773780 @default.
- W2506463670 creator A5032582083 @default.
- W2506463670 creator A5037158086 @default.
- W2506463670 creator A5049584223 @default.
- W2506463670 creator A5069913800 @default.
- W2506463670 creator A5073568638 @default.
- W2506463670 creator A5076332622 @default.
- W2506463670 creator A5088088870 @default.
- W2506463670 date "2016-08-19" @default.
- W2506463670 modified "2023-10-17" @default.
- W2506463670 title "Deepwater circulation variation in the South China Sea since the Last Glacial Maximum" @default.
- W2506463670 cites W139320088 @default.
- W2506463670 cites W1567677637 @default.
- W2506463670 cites W1573547234 @default.
- W2506463670 cites W1770855718 @default.
- W2506463670 cites W1804577523 @default.
- W2506463670 cites W1898956105 @default.
- W2506463670 cites W1939099191 @default.
- W2506463670 cites W1967838752 @default.
- W2506463670 cites W1972925337 @default.
- W2506463670 cites W1978928221 @default.
- W2506463670 cites W1979605699 @default.
- W2506463670 cites W1980818108 @default.
- W2506463670 cites W1984484080 @default.
- W2506463670 cites W1987229149 @default.
- W2506463670 cites W1987439838 @default.
- W2506463670 cites W1988661126 @default.
- W2506463670 cites W1989676793 @default.
- W2506463670 cites W1989820830 @default.
- W2506463670 cites W1990046601 @default.
- W2506463670 cites W1992982340 @default.
- W2506463670 cites W1993809778 @default.
- W2506463670 cites W1995471679 @default.
- W2506463670 cites W1996999479 @default.
- W2506463670 cites W1999814542 @default.
- W2506463670 cites W2002717773 @default.
- W2506463670 cites W2003868383 @default.
- W2506463670 cites W2008875043 @default.
- W2506463670 cites W2013430677 @default.
- W2506463670 cites W2014727327 @default.
- W2506463670 cites W2017024367 @default.
- W2506463670 cites W2019994632 @default.
- W2506463670 cites W2023542692 @default.
- W2506463670 cites W2027055142 @default.
- W2506463670 cites W2027348709 @default.
- W2506463670 cites W2033619635 @default.
- W2506463670 cites W2039437716 @default.
- W2506463670 cites W2043942893 @default.
- W2506463670 cites W2050915907 @default.
- W2506463670 cites W2055132754 @default.
- W2506463670 cites W2067001286 @default.
- W2506463670 cites W2072358065 @default.
- W2506463670 cites W2073325948 @default.
- W2506463670 cites W2074379113 @default.
- W2506463670 cites W2074482550 @default.
- W2506463670 cites W2078805101 @default.
- W2506463670 cites W2079549096 @default.
- W2506463670 cites W2093904312 @default.
- W2506463670 cites W2095477341 @default.
- W2506463670 cites W2096179172 @default.
- W2506463670 cites W2096511474 @default.
- W2506463670 cites W2099667979 @default.
- W2506463670 cites W2103600357 @default.
- W2506463670 cites W2120686284 @default.
- W2506463670 cites W2127150857 @default.
- W2506463670 cites W2148362593 @default.
- W2506463670 cites W2171488289 @default.
- W2506463670 cites W2176978061 @default.
- W2506463670 cites W2177083907 @default.
- W2506463670 cites W2333348788 @default.
- W2506463670 cites W4255338144 @default.
- W2506463670 doi "https://doi.org/10.1002/2016gl070342" @default.
- W2506463670 hasPublicationYear "2016" @default.
- W2506463670 type Work @default.
- W2506463670 sameAs 2506463670 @default.
- W2506463670 citedByCount "30" @default.
- W2506463670 countsByYear W25064636702017 @default.
- W2506463670 countsByYear W25064636702018 @default.
- W2506463670 countsByYear W25064636702019 @default.
- W2506463670 countsByYear W25064636702020 @default.
- W2506463670 countsByYear W25064636702021 @default.
- W2506463670 countsByYear W25064636702022 @default.
- W2506463670 countsByYear W25064636702023 @default.
- W2506463670 crossrefType "journal-article" @default.
- W2506463670 hasAuthorship W2506463670A5000033732 @default.
- W2506463670 hasAuthorship W2506463670A5004586541 @default.
- W2506463670 hasAuthorship W2506463670A5014186251 @default.
- W2506463670 hasAuthorship W2506463670A5024507723 @default.
- W2506463670 hasAuthorship W2506463670A5024878311 @default.
- W2506463670 hasAuthorship W2506463670A5027773780 @default.
- W2506463670 hasAuthorship W2506463670A5032582083 @default.