FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2072630381> ?p ?o ?g. }

• W2072630381 abstract "[1] The preindustrial carbon cycle is described for the Canadian Centre for Climate Modelling and Analysis Earth system model (CanESM1). The interhemispheric gradient of surface atmospheric CO2 concentration (xCO2) is reversed from the present day, with higher concentrations in the Southern Hemisphere, and southward interhemispheric transport by the ocean, estimated at 0.38 Pg C yr−1. The seasonal cycles of xCO2 and surface CO2 exchange are dominated by Northern Hemisphere terrestrial processes; the ocean contribution to CO2 flux is in phase with the larger terrestrial flux in the tropics and out of phase in the extratropics. Ocean processes dominate the relatively small Southern Hemisphere variability. Interannual variability of land carbon exchange is much larger than ocean exchange; both are comparable to results from previously published models with possibly larger variability in the terrestrial flux. Terrestrial net primary production (NPP) is determined largely by water availability at low latitudes, with temperature becoming more important at high latitudes. Temperature and moisture affect both NPP and heterotrophic respiration such that respiration effects tend to dampen the effect of fluctuations in NPP on CO2 exchange. Ocean CO2 flux variability is controlled by a variety of physical and biological processes with greater control by physical processes in the tropics and a larger biological contribution in the extratropics. Ocean CO2 flux is more strongly correlated with tropical sea surface temperature (SST) than terrestrial, but the variance associated with tropical SST is larger on land, in absolute terms, because of the much greater total variance of the land carbon flux. A novel hypothesis is advanced to explain how biological drawdown can cause recently upwelled water to be a net sink rather than source for atmospheric CO2. This process occurs over large areas of extratropical ocean and forms a natural sink for atmospheric CO2 that is potentially sensitive to both ocean acidification and anthropogenic perturbations of the aeolian iron flux." @default.
• W2072630381 created "2016-06-24" @default.
• W2072630381 creator A5006311305 @default.
• W2072630381 creator A5026161312 @default.
• W2072630381 creator A5026720516 @default.
• W2072630381 creator A5035374502 @default.
• W2072630381 creator A5042274089 @default.
• W2072630381 creator A5053861379 @default.
• W2072630381 creator A5054091795 @default.
• W2072630381 creator A5057168744 @default.
• W2072630381 creator A5072258957 @default.
• W2072630381 creator A5083446207 @default.
• W2072630381 creator A5083536933 @default.
• W2072630381 date "2010-08-17" @default.
• W2072630381 modified "2023-10-09" @default.
• W2072630381 title "The global carbon cycle in the Canadian Earth system model (CanESM1): Preindustrial control simulation" @default.
• W2072630381 cites W1559564413 @default.
• W2072630381 cites W1600578893 @default.
• W2072630381 cites W1609491364 @default.
• W2072630381 cites W1674831397 @default.
• W2072630381 cites W1859438061 @default.
• W2072630381 cites W1966089332 @default.
• W2072630381 cites W1970468918 @default.
• W2072630381 cites W1971689107 @default.
• W2072630381 cites W1975352576 @default.
• W2072630381 cites W1977892071 @default.
• W2072630381 cites W1985218331 @default.
• W2072630381 cites W1992073696 @default.
• W2072630381 cites W1992837490 @default.
• W2072630381 cites W1992957327 @default.
• W2072630381 cites W1994654469 @default.
• W2072630381 cites W1999864011 @default.
• W2072630381 cites W2003746676 @default.
• W2072630381 cites W2006583314 @default.
• W2072630381 cites W2009280131 @default.
• W2072630381 cites W2010120786 @default.
• W2072630381 cites W2011374672 @default.
• W2072630381 cites W2011601793 @default.
• W2072630381 cites W2013537840 @default.
• W2072630381 cites W2017870133 @default.
• W2072630381 cites W2026245108 @default.
• W2072630381 cites W2026713732 @default.
• W2072630381 cites W2026865113 @default.
• W2072630381 cites W2028938077 @default.
• W2072630381 cites W2029074727 @default.
• W2072630381 cites W2029822020 @default.
• W2072630381 cites W2035888601 @default.
• W2072630381 cites W2040215001 @default.
• W2072630381 cites W2043236414 @default.
• W2072630381 cites W2045036691 @default.
• W2072630381 cites W2046857879 @default.
• W2072630381 cites W2048711169 @default.
• W2072630381 cites W2052022886 @default.
• W2072630381 cites W2057858033 @default.
• W2072630381 cites W2060097988 @default.
• W2072630381 cites W2062778690 @default.
• W2072630381 cites W2074458860 @default.
• W2072630381 cites W2076254337 @default.
• W2072630381 cites W2093065735 @default.
• W2072630381 cites W2093401535 @default.
• W2072630381 cites W2094226391 @default.
• W2072630381 cites W2104663801 @default.
• W2072630381 cites W2110293632 @default.
• W2072630381 cites W2111224249 @default.
• W2072630381 cites W2115813766 @default.
• W2072630381 cites W2118440730 @default.
• W2072630381 cites W2122800143 @default.
• W2072630381 cites W2126860661 @default.
• W2072630381 cites W2135082344 @default.
• W2072630381 cites W2136188488 @default.
• W2072630381 cites W2147810057 @default.
• W2072630381 cites W2151328940 @default.
• W2072630381 cites W2156076254 @default.
• W2072630381 cites W2158140310 @default.
• W2072630381 cites W2162013661 @default.
• W2072630381 cites W2162302470 @default.
• W2072630381 cites W2163897408 @default.
• W2072630381 cites W2173970595 @default.
• W2072630381 doi "https://doi.org/10.1029/2008jg000920" @default.
• W2072630381 hasPublicationYear "2010" @default.
• W2072630381 type Work @default.
• W2072630381 sameAs 2072630381 @default.
• W2072630381 citedByCount "60" @default.
• W2072630381 countsByYear W20726303812012 @default.
• W2072630381 countsByYear W20726303812013 @default.
• W2072630381 countsByYear W20726303812014 @default.
• W2072630381 countsByYear W20726303812015 @default.
• W2072630381 countsByYear W20726303812016 @default.
• W2072630381 countsByYear W20726303812017 @default.
• W2072630381 countsByYear W20726303812018 @default.
• W2072630381 countsByYear W20726303812019 @default.
• W2072630381 countsByYear W20726303812020 @default.
• W2072630381 countsByYear W20726303812021 @default.
• W2072630381 countsByYear W20726303812022 @default.
• W2072630381 countsByYear W20726303812023 @default.
• W2072630381 crossrefType "journal-article" @default.
• W2072630381 hasAuthorship W2072630381A5006311305 @default.
• W2072630381 hasAuthorship W2072630381A5026161312 @default.
• W2072630381 hasAuthorship W2072630381A5026720516 @default.
• W2072630381 hasAuthorship W2072630381A5035374502 @default.

• next