FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2130378296> ?p ?o ?g. }

• W2130378296 abstract "Between 1983 and 2005, continuous oceanic CO 2 observations at two time series sites in the North Atlantic Ocean near Bermuda indicate that surface seawater dissolved inorganic carbon (DIC) and p CO 2 increased annually at rates similar to that expected from oceanic equilibration with increasing CO 2 in the atmosphere. In addition, seawater p H, CO 3 2− ion concentrations, and CaCO 3 saturation states have also decreased over time. There was considerable seasonal asymmetry in the oceanic CO 2 sink or source rates, with wintertime air‐to‐sea CO 2 influx greater than the summertime sea‐to‐air CO 2 efflux. On an annual basis, the region was an oceanic sink for CO 2 , with a mean net annual air‐sea CO 2 flux rate of −815 ± 251 and −1295 ± 294 mmol CO 2 m −2 yr −1 , respectively, estimated using different synoptic and data assimilation model wind speed data sets. Peak‐to‐peak variability of ∼850–1950 mmol CO 2 m −2 yr −1 represented an interannual variability of ∼0.2–0.3 Pg C yr −1 in the oceanic CO 2 sink scaled to the subtropical gyre of North Atlantic Ocean. The long‐term trend over the 1983–2005 period was a slight increase in the oceanic CO 2 sink, associated primarily with a gradual increase in wind speed over the same period. Interannual variability of summertime (June–September) and fall (October–December) air‐sea CO 2 flux rates were correlated to the North Atlantic Oscillation (NAO) and strongly influenced by wind events such as hurricanes. Wintertime (January–May) air‐sea CO 2 flux rates were poorly correlated with the NAO and Arctic Oscillation (AO), although gas exchange rates were ∼11–40% higher during concurrent El Niño periods compared to La Niña periods." @default.
• W2130378296 created "2016-06-24" @default.
• W2130378296 creator A5041217929 @default.
• W2130378296 date "2007-09-01" @default.
• W2130378296 modified "2023-10-17" @default.
• W2130378296 title "Interannual variability of the oceanic CO₂sink in the subtropical gyre of the North Atlantic Ocean over the last 2 decades" @default.
• W2130378296 cites W1174483205 @default.
• W2130378296 cites W1486870715 @default.
• W2130378296 cites W1513196349 @default.
• W2130378296 cites W1515234455 @default.
• W2130378296 cites W1540182902 @default.
• W2130378296 cites W1550730432 @default.
• W2130378296 cites W1560596117 @default.
• W2130378296 cites W1567905987 @default.
• W2130378296 cites W1586973386 @default.
• W2130378296 cites W1608720283 @default.
• W2130378296 cites W1624413182 @default.
• W2130378296 cites W1626271904 @default.
• W2130378296 cites W1681234379 @default.
• W2130378296 cites W1963711128 @default.
• W2130378296 cites W1964685761 @default.
• W2130378296 cites W1968655655 @default.
• W2130378296 cites W1969184914 @default.
• W2130378296 cites W1979011173 @default.
• W2130378296 cites W1979102222 @default.
• W2130378296 cites W1980177490 @default.
• W2130378296 cites W1981320163 @default.
• W2130378296 cites W1981542592 @default.
• W2130378296 cites W1983275003 @default.
• W2130378296 cites W1984006825 @default.
• W2130378296 cites W1986954778 @default.
• W2130378296 cites W1994708721 @default.
• W2130378296 cites W1995349031 @default.
• W2130378296 cites W1999314426 @default.
• W2130378296 cites W2001223907 @default.
• W2130378296 cites W2002968001 @default.
• W2130378296 cites W2007849811 @default.
• W2130378296 cites W2011051057 @default.
• W2130378296 cites W2014236192 @default.
• W2130378296 cites W2014458241 @default.
• W2130378296 cites W2018516735 @default.
• W2130378296 cites W2020297738 @default.
• W2130378296 cites W2020712598 @default.
• W2130378296 cites W2023057352 @default.
• W2130378296 cites W2028063827 @default.
• W2130378296 cites W2029762335 @default.
• W2130378296 cites W2030604405 @default.
• W2130378296 cites W2034381881 @default.
• W2130378296 cites W2035468030 @default.
• W2130378296 cites W2038259434 @default.
• W2130378296 cites W2043390964 @default.
• W2130378296 cites W2045035085 @default.
• W2130378296 cites W2047321122 @default.
• W2130378296 cites W2055338027 @default.
• W2130378296 cites W2060012482 @default.
• W2130378296 cites W2060392698 @default.
• W2130378296 cites W2061002844 @default.
• W2130378296 cites W2062826995 @default.
• W2130378296 cites W2063572919 @default.
• W2130378296 cites W2064634195 @default.
• W2130378296 cites W2064773850 @default.
• W2130378296 cites W2065080850 @default.
• W2130378296 cites W2067910389 @default.
• W2130378296 cites W2068290737 @default.
• W2130378296 cites W2069033887 @default.
• W2130378296 cites W2069976252 @default.
• W2130378296 cites W2070050109 @default.
• W2130378296 cites W2072749934 @default.
• W2130378296 cites W2073339546 @default.
• W2130378296 cites W2073721556 @default.
• W2130378296 cites W2073885728 @default.
• W2130378296 cites W2077258558 @default.
• W2130378296 cites W2080553218 @default.
• W2130378296 cites W2081227951 @default.
• W2130378296 cites W2081961197 @default.
• W2130378296 cites W2082291024 @default.
• W2130378296 cites W2085285331 @default.
• W2130378296 cites W2086290934 @default.
• W2130378296 cites W2090668823 @default.
• W2130378296 cites W2090907235 @default.
• W2130378296 cites W2091390908 @default.
• W2130378296 cites W2091945915 @default.
• W2130378296 cites W2092277183 @default.
• W2130378296 cites W2092458314 @default.
• W2130378296 cites W2094300388 @default.
• W2130378296 cites W2094845411 @default.
• W2130378296 cites W2100959277 @default.
• W2130378296 cites W2104580694 @default.
• W2130378296 cites W2106912447 @default.
• W2130378296 cites W2110725762 @default.
• W2130378296 cites W2111549347 @default.
• W2130378296 cites W2112435983 @default.
• W2130378296 cites W2118086939 @default.
• W2130378296 cites W2119844460 @default.
• W2130378296 cites W2120991774 @default.
• W2130378296 cites W2125416759 @default.
• W2130378296 cites W2125776675 @default.
• W2130378296 cites W2129203694 @default.
• W2130378296 cites W2131477567 @default.
• W2130378296 cites W2140374314 @default.

• next