FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2029596959> ?p ?o ?g. }

• W2029596959 endingPage "23083" @default.
• W2029596959 startingPage "23083" @default.
• W2029596959 abstract "We estimate regional long-term surface ocean pCO2 growth rates using all available underway and bottled biogeochemistry data collected over the past four decades. These observed regional trends are compared with those simulated by five state-of-the-art Earth system models over the historical period. Oceanic pCO2 growth rates faster than the atmospheric growth rates indicate decreasing atmospheric CO2 uptake, while ocean pCO2 growth rates slower than the atmospheric growth rates indicate increasing atmospheric CO2 uptake. Aside from the western subpolar North Pacific and the subtropical North Atlantic, our analysis indicates that the current observation-based basin-scale trends may be underestimated, indicating that more observations are needed to determine the trends in these regions. Encouragingly, good agreement between the simulated and observed pCO2 trends is found when the simulated fields are subsampled with the observational coverage. In agreement with observations, we see that the simulated pCO2 trends are primarily associated with the increase in surface dissolved inorganic carbon (DIC) associated with atmospheric carbon uptake, and in part by warming of the sea surface. Under the RCP8.5 future scenario, DIC continues to be the dominant driver of pCO2 trends, with little change in the relative contribution of SST. However, the changes in the hydrological cycle play an increasingly important role. For the contemporary (1970–2011) period, the simulated regional pCO2 trends are lower than the atmospheric growth rate over 90% of the ocean. However, by year 2100 more than 40% of the surface ocean area has a higher oceanic pCO2 trend than the atmosphere, implying a reduction in the atmospheric CO2 uptake rate. The fastest pCO2 growth rates are projected for the subpolar North Atlantic, while the high-latitude Southern Ocean and eastern equatorial Pacific have the weakest growth rates, remaining below the atmospheric pCO2 growth rate. Our work also highlights the importance and need for a sustained long-term observing strategy to continue monitoring the change in the ocean anthropogenic CO2 sink and to better understand the potential carbon cycle feedbacks to climate that could arise from it." @default.
• W2029596959 created "2016-06-24" @default.
• W2029596959 creator A5012320872 @default.
• W2029596959 creator A5032040763 @default.
• W2029596959 creator A5041681983 @default.
• W2029596959 creator A5050524996 @default.
• W2029596959 creator A5056263151 @default.
• W2029596959 creator A5063959948 @default.
• W2029596959 creator A5077512301 @default.
• W2029596959 creator A5079839995 @default.
• W2029596959 creator A5083109543 @default.
• W2029596959 date "2014-01-01" @default.
• W2029596959 modified "2023-10-16" @default.
• W2029596959 title "Long-term surface pCO₂ trends from observations and models" @default.
• W2029596959 cites W1480868893 @default.
• W2029596959 cites W1507989638 @default.
• W2029596959 cites W1521371173 @default.
• W2029596959 cites W1559564413 @default.
• W2029596959 cites W1587310363 @default.
• W2029596959 cites W1596017335 @default.
• W2029596959 cites W1608098346 @default.
• W2029596959 cites W1685359561 @default.
• W2029596959 cites W1717270090 @default.
• W2029596959 cites W1976264057 @default.
• W2029596959 cites W1982831135 @default.
• W2029596959 cites W1989141253 @default.
• W2029596959 cites W2002545808 @default.
• W2029596959 cites W2008291590 @default.
• W2029596959 cites W2009117726 @default.
• W2029596959 cites W2024966118 @default.
• W2029596959 cites W2030604405 @default.
• W2029596959 cites W2045329005 @default.
• W2029596959 cites W2049797375 @default.
• W2029596959 cites W2053867554 @default.
• W2029596959 cites W2063534846 @default.
• W2029596959 cites W2072653423 @default.
• W2029596959 cites W2077330513 @default.
• W2029596959 cites W2078355831 @default.
• W2029596959 cites W2080395149 @default.
• W2029596959 cites W2106846981 @default.
• W2029596959 cites W2108208049 @default.
• W2029596959 cites W2114653148 @default.
• W2029596959 cites W2125121685 @default.
• W2029596959 cites W2125776675 @default.
• W2029596959 cites W2130341490 @default.
• W2029596959 cites W2130434897 @default.
• W2029596959 cites W2135261232 @default.
• W2029596959 cites W2135542541 @default.
• W2029596959 cites W2135725459 @default.
• W2029596959 cites W2137034930 @default.
• W2029596959 cites W2141707502 @default.
• W2029596959 cites W2143487353 @default.
• W2029596959 cites W2145255150 @default.
• W2029596959 cites W2154356323 @default.
• W2029596959 cites W2161454991 @default.
• W2029596959 cites W2163502526 @default.
• W2029596959 cites W2163944093 @default.
• W2029596959 doi "https://doi.org/10.3402/tellusb.v66.23083" @default.
• W2029596959 hasPublicationYear "2014" @default.
• W2029596959 type Work @default.
• W2029596959 sameAs 2029596959 @default.
• W2029596959 citedByCount "43" @default.
• W2029596959 countsByYear W20295969592014 @default.
• W2029596959 countsByYear W20295969592015 @default.
• W2029596959 countsByYear W20295969592016 @default.
• W2029596959 countsByYear W20295969592018 @default.
• W2029596959 countsByYear W20295969592019 @default.
• W2029596959 countsByYear W20295969592020 @default.
• W2029596959 countsByYear W20295969592021 @default.
• W2029596959 countsByYear W20295969592022 @default.
• W2029596959 countsByYear W20295969592023 @default.
• W2029596959 crossrefType "journal-article" @default.
• W2029596959 hasAuthorship W2029596959A5012320872 @default.
• W2029596959 hasAuthorship W2029596959A5032040763 @default.
• W2029596959 hasAuthorship W2029596959A5041681983 @default.
• W2029596959 hasAuthorship W2029596959A5050524996 @default.
• W2029596959 hasAuthorship W2029596959A5056263151 @default.
• W2029596959 hasAuthorship W2029596959A5063959948 @default.
• W2029596959 hasAuthorship W2029596959A5077512301 @default.
• W2029596959 hasAuthorship W2029596959A5079839995 @default.
• W2029596959 hasAuthorship W2029596959A5083109543 @default.
• W2029596959 hasBestOaLocation W20295969591 @default.
• W2029596959 hasConcept C111368507 @default.
• W2029596959 hasConcept C127313418 @default.
• W2029596959 hasConcept C130309983 @default.
• W2029596959 hasConcept C132651083 @default.
• W2029596959 hasConcept C134097258 @default.
• W2029596959 hasConcept C153294291 @default.
• W2029596959 hasConcept C195048187 @default.
• W2029596959 hasConcept C205649164 @default.
• W2029596959 hasConcept C39432304 @default.
• W2029596959 hasConcept C49204034 @default.
• W2029596959 hasConcept C65440619 @default.
• W2029596959 hasConcept C91586092 @default.
• W2029596959 hasConceptScore W2029596959C111368507 @default.
• W2029596959 hasConceptScore W2029596959C127313418 @default.
• W2029596959 hasConceptScore W2029596959C130309983 @default.
• W2029596959 hasConceptScore W2029596959C132651083 @default.

• next