Matches in SemOpenAlex for { <https://semopenalex.org/work/W577822999> ?p ?o ?g. }
- W577822999 endingPage "109" @default.
- W577822999 startingPage "98" @default.
- W577822999 abstract "The deep and surface water paleoceanographic evolution of the central Nordic Seas over the last 20 thousand years was reconstructed using various micropaleontological, isotopic and lithological proxy data. These show a high spatial and temporal complexity of the oceanic circulation when compared with other records from the region. During early deglaciation a collapse of ice sheets surrounding the Nordic Seas released large amounts of freshwater that affected both the surface and bottom water circulation and significantly contributed to Heinrich stadial 1. During the Younger Dryas, the central Nordic Seas were affected by a last major freshwater plume which probably originated from the Arctic Ocean. When major ice rafting had ceased around 11ka subsurface temperatures started to rise. However, Atlantic Water advection and subsurface temperatures reached their maximum in the central Nordic Seas later than along the eastern continental margin. That spatio-temporal offset is explained by a gradual re-routing and westward expansion of the Atlantic Water flow during times when the Greenland Sea gyre system became more steadily established. In the Greenland Basin, the Holocene thermal maximum ended c. 5.5ka, and time-coeveal with an increase in sea-ice export from the Arctic. In the Lofoten Basin the cooling occurred later, after 4ka, and together with a weakening of the overturning processes. The Neoglacial cooling was reached c. 3ka, together with low solar irradiance, expanding sea ice and a slight decrease in deep convection. At c. 2ka subsurface temperatures began to rise again due to an increasing influence of Atlantic Waters." @default.
- W577822999 created "2016-06-24" @default.
- W577822999 creator A5011837454 @default.
- W577822999 creator A5056552289 @default.
- W577822999 creator A5078582269 @default.
- W577822999 creator A5078924116 @default.
- W577822999 date "2015-08-01" @default.
- W577822999 modified "2023-09-26" @default.
- W577822999 title "Evolution of the central Nordic Seas over the last 20 thousand years" @default.
- W577822999 cites W1488051296 @default.
- W577822999 cites W1499565783 @default.
- W577822999 cites W1524211435 @default.
- W577822999 cites W1581622930 @default.
- W577822999 cites W1602069029 @default.
- W577822999 cites W163198 @default.
- W577822999 cites W1639268213 @default.
- W577822999 cites W1646758270 @default.
- W577822999 cites W1656848733 @default.
- W577822999 cites W1835990359 @default.
- W577822999 cites W1897950478 @default.
- W577822999 cites W1941353130 @default.
- W577822999 cites W1964997552 @default.
- W577822999 cites W1971228562 @default.
- W577822999 cites W1975324062 @default.
- W577822999 cites W1975887308 @default.
- W577822999 cites W1982002268 @default.
- W577822999 cites W1983844230 @default.
- W577822999 cites W1985167833 @default.
- W577822999 cites W1986513960 @default.
- W577822999 cites W1987067034 @default.
- W577822999 cites W1987439838 @default.
- W577822999 cites W1995248692 @default.
- W577822999 cites W1995613894 @default.
- W577822999 cites W1996862213 @default.
- W577822999 cites W1997672855 @default.
- W577822999 cites W1999027888 @default.
- W577822999 cites W2002517276 @default.
- W577822999 cites W2002717773 @default.
- W577822999 cites W2005786608 @default.
- W577822999 cites W2013686371 @default.
- W577822999 cites W2020414925 @default.
- W577822999 cites W2020877823 @default.
- W577822999 cites W2024032157 @default.
- W577822999 cites W2035723148 @default.
- W577822999 cites W2036640985 @default.
- W577822999 cites W2039819271 @default.
- W577822999 cites W2043672520 @default.
- W577822999 cites W2044438318 @default.
- W577822999 cites W2045052711 @default.
- W577822999 cites W2046913473 @default.
- W577822999 cites W2050597567 @default.
- W577822999 cites W2051126029 @default.
- W577822999 cites W2054307300 @default.
- W577822999 cites W2054410181 @default.
- W577822999 cites W2055184764 @default.
- W577822999 cites W2055615694 @default.
- W577822999 cites W2063401228 @default.
- W577822999 cites W2063812989 @default.
- W577822999 cites W2070753499 @default.
- W577822999 cites W2071243999 @default.
- W577822999 cites W2073823102 @default.
- W577822999 cites W2073926840 @default.
- W577822999 cites W2074527287 @default.
- W577822999 cites W2080444208 @default.
- W577822999 cites W2081968403 @default.
- W577822999 cites W2082513665 @default.
- W577822999 cites W2083528729 @default.
- W577822999 cites W2084428435 @default.
- W577822999 cites W2087625531 @default.
- W577822999 cites W2088206730 @default.
- W577822999 cites W2093468243 @default.
- W577822999 cites W2094369396 @default.
- W577822999 cites W2099063201 @default.
- W577822999 cites W2099727517 @default.
- W577822999 cites W2103737089 @default.
- W577822999 cites W2104040517 @default.
- W577822999 cites W2104490095 @default.
- W577822999 cites W2106102617 @default.
- W577822999 cites W2107917625 @default.
- W577822999 cites W2108814505 @default.
- W577822999 cites W2112005698 @default.
- W577822999 cites W2121138676 @default.
- W577822999 cites W2128614169 @default.
- W577822999 cites W2132751006 @default.
- W577822999 cites W2142664760 @default.
- W577822999 cites W2143508175 @default.
- W577822999 cites W2145926945 @default.
- W577822999 cites W2149976868 @default.
- W577822999 cites W2152666315 @default.
- W577822999 cites W2158271855 @default.
- W577822999 cites W2158918602 @default.
- W577822999 cites W2161160541 @default.
- W577822999 cites W2280624662 @default.
- W577822999 cites W4238289388 @default.
- W577822999 cites W4249751050 @default.
- W577822999 doi "https://doi.org/10.1016/j.quascirev.2015.05.013" @default.
- W577822999 hasPublicationYear "2015" @default.
- W577822999 type Work @default.