Matches in SemOpenAlex for { <https://semopenalex.org/work/W2103644013> ?p ?o ?g. }
- W2103644013 endingPage "999" @default.
- W2103644013 startingPage "984" @default.
- W2103644013 abstract "Abstract The complex deglacial to Holocene oceanographic development in the Gulf of Guayaquil (Eastern Equatorial Pacific) is reconstructed for sea surface and subsurface ocean levels from (isotope) geochemical proxies based on marine sediment cores. At sea surface, southern sourced Cold Coastal Water and tropical Equatorial Surface Water/Tropical Surface Water are intimately related. In particular since ~10 ka, independent sea surface temperature proxies capturing different seasons emphasize the growing seasonal contrast in the Gulf of Guayaquil, which is in contrast to ocean areas further offshore. Cold Coastal Water became rapidly present in the Gulf of Guayaquil during the austral winter season in line with the strengthening of the Southeast Trades, while coastal upwelling off Peru gradually intensified and expanded northward in response to a seasonally changing atmospheric circulation pattern affecting the core locations intensively since 4 ka BP. Equatorial Surface Water, instead, was displaced and Tropical Surface Water moved northward together with the Equatorial Front. At subsurface, the presence of Equatorial Under Current‐sourced Equatorial Subsurface Water was continuously growing, prominently since ~10–8 ka B.P. During Heinrich Stadial 1 and large parts of the Bølling/Allerød, and similarly during short Holocene time intervals at ~5.1–4 ka B.P. and ~1.5–0.5 ka B.P., the admixture of Equatorial Subsurface Water was reduced in response to both short‐term weakening of Equatorial Under Current strength from the northwest and emplacement by tropical Equatorial Surface Water, considerably warming the uppermost ocean layers." @default.
- W2103644013 created "2016-06-24" @default.
- W2103644013 creator A5023674953 @default.
- W2103644013 creator A5035876154 @default.
- W2103644013 creator A5050713145 @default.
- W2103644013 creator A5063234196 @default.
- W2103644013 creator A5079855584 @default.
- W2103644013 creator A5090277832 @default.
- W2103644013 date "2015-07-01" @default.
- W2103644013 modified "2023-10-17" @default.
- W2103644013 title "Sea surface and subsurface circulation dynamics off equatorial Peru during the last ~17 kyr" @default.
- W2103644013 cites W1582736910 @default.
- W2103644013 cites W1601300385 @default.
- W2103644013 cites W1603972355 @default.
- W2103644013 cites W1768354679 @default.
- W2103644013 cites W1770994388 @default.
- W2103644013 cites W1842683167 @default.
- W2103644013 cites W1893787057 @default.
- W2103644013 cites W1916565667 @default.
- W2103644013 cites W1938526285 @default.
- W2103644013 cites W1953339068 @default.
- W2103644013 cites W1966282214 @default.
- W2103644013 cites W1968588988 @default.
- W2103644013 cites W1973776704 @default.
- W2103644013 cites W1976335483 @default.
- W2103644013 cites W1982058488 @default.
- W2103644013 cites W1986494512 @default.
- W2103644013 cites W1989673732 @default.
- W2103644013 cites W1990669782 @default.
- W2103644013 cites W1991916332 @default.
- W2103644013 cites W1992818746 @default.
- W2103644013 cites W1997626537 @default.
- W2103644013 cites W1999224121 @default.
- W2103644013 cites W2005157044 @default.
- W2103644013 cites W2009583290 @default.
- W2103644013 cites W2017004431 @default.
- W2103644013 cites W2029598829 @default.
- W2103644013 cites W2031519953 @default.
- W2103644013 cites W2035587516 @default.
- W2103644013 cites W2037580998 @default.
- W2103644013 cites W2037780479 @default.
- W2103644013 cites W2040180267 @default.
- W2103644013 cites W2042077234 @default.
- W2103644013 cites W2046035856 @default.
- W2103644013 cites W2048763271 @default.
- W2103644013 cites W2052066227 @default.
- W2103644013 cites W2053403427 @default.
- W2103644013 cites W2067183885 @default.
- W2103644013 cites W2068201483 @default.
- W2103644013 cites W2068207047 @default.
- W2103644013 cites W2071510155 @default.
- W2103644013 cites W2071868028 @default.
- W2103644013 cites W2072843931 @default.
- W2103644013 cites W2074190811 @default.
- W2103644013 cites W2075250643 @default.
- W2103644013 cites W2075385168 @default.
- W2103644013 cites W2076850342 @default.
- W2103644013 cites W2079500758 @default.
- W2103644013 cites W2090162946 @default.
- W2103644013 cites W2093174650 @default.
- W2103644013 cites W2095425585 @default.
- W2103644013 cites W2105454455 @default.
- W2103644013 cites W2110433503 @default.
- W2103644013 cites W2110783004 @default.
- W2103644013 cites W2112169783 @default.
- W2103644013 cites W2115201009 @default.
- W2103644013 cites W2116367889 @default.
- W2103644013 cites W2122858006 @default.
- W2103644013 cites W2123241285 @default.
- W2103644013 cites W2125835805 @default.
- W2103644013 cites W2125862277 @default.
- W2103644013 cites W2136012436 @default.
- W2103644013 cites W2139559492 @default.
- W2103644013 cites W2139735175 @default.
- W2103644013 cites W2147017368 @default.
- W2103644013 cites W2151820098 @default.
- W2103644013 cites W2151952626 @default.
- W2103644013 cites W2154128128 @default.
- W2103644013 cites W2159447010 @default.
- W2103644013 cites W2170427783 @default.
- W2103644013 cites W2477221022 @default.
- W2103644013 cites W2506821467 @default.
- W2103644013 cites W254570906 @default.
- W2103644013 cites W4297979764 @default.
- W2103644013 cites W766046272 @default.
- W2103644013 doi "https://doi.org/10.1002/2014pa002706" @default.
- W2103644013 hasPublicationYear "2015" @default.
- W2103644013 type Work @default.
- W2103644013 sameAs 2103644013 @default.
- W2103644013 citedByCount "24" @default.
- W2103644013 countsByYear W21036440132015 @default.
- W2103644013 countsByYear W21036440132016 @default.
- W2103644013 countsByYear W21036440132017 @default.
- W2103644013 countsByYear W21036440132018 @default.
- W2103644013 countsByYear W21036440132019 @default.
- W2103644013 countsByYear W21036440132020 @default.
- W2103644013 countsByYear W21036440132021 @default.
- W2103644013 countsByYear W21036440132022 @default.