FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3169673908> ?p ?o ?g. }

• W3169673908 abstract "Abstract Model intercomparison studies of coupled carbon‐climate simulations have the potential to improve our understanding of the processes explaining the drawdown at the Last Glacial Maximum (LGM) and to identify related model biases. Models participating in the Paleoclimate Modeling Intercomparison Project (PMIP) now frequently include the carbon cycle. The ongoing PMIP‐carbon project provides the first opportunity to conduct multimodel comparisons of simulated carbon content for the LGM time window. However, such a study remains challenging due to differing implementation of ocean boundary conditions (e.g., bathymetry and coastlines reflecting the low sea level) and to various associated adjustments of biogeochemical variables (i.e., alkalinity, nutrients, dissolved inorganic carbon). After assessing the ocean volume of PMIP models at the pre‐industrial and LGM, we investigate the impact of these modeling choices on the simulated carbon at the global scale, using both PMIP‐carbon model outputs and sensitivity tests with the iLOVECLIM model. We show that the carbon distribution in reservoirs is significantly affected by the choice of ocean boundary conditions in iLOVECLIM. In particular, our simulations demonstrate a GtC effect of an alkalinity adjustment on carbon sequestration in the ocean. Finally, we observe that PMIP‐carbon models with a freely evolving and no additional glacial mechanisms do not simulate the drawdown at the LGM (with concentrations as high as 313, 331, and 315 ppm), especially if they use a low ocean volume. Our findings suggest that great care should be taken on accounting for large bathymetry changes in models including the carbon cycle." @default.
• W3169673908 created "2021-06-22" @default.
• W3169673908 creator A5004009030 @default.
• W3169673908 creator A5008038356 @default.
• W3169673908 creator A5009454460 @default.
• W3169673908 creator A5018398159 @default.
• W3169673908 creator A5019071655 @default.
• W3169673908 creator A5019517910 @default.
• W3169673908 creator A5023883504 @default.
• W3169673908 creator A5025230059 @default.
• W3169673908 creator A5034808833 @default.
• W3169673908 creator A5039577948 @default.
• W3169673908 creator A5041540294 @default.
• W3169673908 creator A5042278189 @default.
• W3169673908 creator A5053393105 @default.
• W3169673908 creator A5055243478 @default.
• W3169673908 creator A5057423394 @default.
• W3169673908 creator A5060667876 @default.
• W3169673908 creator A5078938486 @default.
• W3169673908 creator A5085333726 @default.
• W3169673908 date "2021-09-29" @default.
• W3169673908 modified "2023-10-02" @default.
• W3169673908 title "A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions" @default.
• W3169673908 cites W1526009946 @default.
• W3169673908 cites W1562504550 @default.
• W3169673908 cites W1591969145 @default.
• W3169673908 cites W1594282911 @default.
• W3169673908 cites W1657772896 @default.
• W3169673908 cites W1676267467 @default.
• W3169673908 cites W1677073775 @default.
• W3169673908 cites W1785003470 @default.
• W3169673908 cites W1942064222 @default.
• W3169673908 cites W1975790343 @default.
• W3169673908 cites W1989707569 @default.
• W3169673908 cites W2002902271 @default.
• W3169673908 cites W2007446886 @default.
• W3169673908 cites W2011374672 @default.
• W3169673908 cites W2018424764 @default.
• W3169673908 cites W2026736655 @default.
• W3169673908 cites W2048862519 @default.
• W3169673908 cites W2064368240 @default.
• W3169673908 cites W2068534353 @default.
• W3169673908 cites W2071906493 @default.
• W3169673908 cites W2079845015 @default.
• W3169673908 cites W2089542793 @default.
• W3169673908 cites W2094350389 @default.
• W3169673908 cites W2095605097 @default.
• W3169673908 cites W2100461650 @default.
• W3169673908 cites W2106226882 @default.
• W3169673908 cites W2109254022 @default.
• W3169673908 cites W2112363056 @default.
• W3169673908 cites W2122943628 @default.
• W3169673908 cites W2135968678 @default.
• W3169673908 cites W2139143774 @default.
• W3169673908 cites W2150303148 @default.
• W3169673908 cites W2155435132 @default.
• W3169673908 cites W2157236799 @default.
• W3169673908 cites W2157256229 @default.
• W3169673908 cites W2159841602 @default.
• W3169673908 cites W2190124010 @default.
• W3169673908 cites W2248445980 @default.
• W3169673908 cites W2516442054 @default.
• W3169673908 cites W2551686028 @default.
• W3169673908 cites W2591443624 @default.
• W3169673908 cites W2617552295 @default.
• W3169673908 cites W2624454205 @default.
• W3169673908 cites W2763089126 @default.
• W3169673908 cites W2768039127 @default.
• W3169673908 cites W2794245781 @default.
• W3169673908 cites W2887558848 @default.
• W3169673908 cites W2894715735 @default.
• W3169673908 cites W2914853585 @default.
• W3169673908 cites W2921757568 @default.
• W3169673908 cites W2951372365 @default.
• W3169673908 cites W2963986113 @default.
• W3169673908 cites W2979511470 @default.
• W3169673908 cites W2991264897 @default.
• W3169673908 cites W3005718335 @default.
• W3169673908 cites W3024077375 @default.
• W3169673908 cites W3080813169 @default.
• W3169673908 cites W3108556398 @default.
• W3169673908 cites W3133075229 @default.
• W3169673908 cites W3163629062 @default.
• W3169673908 doi "https://doi.org/10.1029/2021pa004302" @default.
• W3169673908 hasPublicationYear "2021" @default.
• W3169673908 type Work @default.
• W3169673908 sameAs 3169673908 @default.
• W3169673908 citedByCount "4" @default.
• W3169673908 countsByYear W31696739082023 @default.
• W3169673908 crossrefType "journal-article" @default.
• W3169673908 hasAuthorship W3169673908A5004009030 @default.
• W3169673908 hasAuthorship W3169673908A5008038356 @default.
• W3169673908 hasAuthorship W3169673908A5009454460 @default.
• W3169673908 hasAuthorship W3169673908A5018398159 @default.
• W3169673908 hasAuthorship W3169673908A5019071655 @default.
• W3169673908 hasAuthorship W3169673908A5019517910 @default.
• W3169673908 hasAuthorship W3169673908A5023883504 @default.
• W3169673908 hasAuthorship W3169673908A5025230059 @default.
• W3169673908 hasAuthorship W3169673908A5034808833 @default.
• W3169673908 hasAuthorship W3169673908A5039577948 @default.

• next