FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3199264342> ?p ?o ?g. }

• W3199264342 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> Exchange of carbon between the ocean and the atmosphere is a key process that influences past climates via glacial–interglacial variations of the <span class=inline-formula>CO₂</span> concentration. The melting of ice sheets during deglaciations induces a sea level rise which leads to the flooding of coastal land areas, resulting in the transfer of terrestrial organic matter to the ocean. However, the consequences of such fluxes on the ocean biogeochemical cycle and on the uptake and release of <span class=inline-formula>CO₂</span> are poorly constrained. Moreover, this potentially important exchange of carbon at the land–sea interface is not represented in most Earth system models. We present here the implementation of terrestrial organic matter fluxes into the ocean at the transiently changing land–sea interface in the Max Planck Institute for Meteorology Earth System Model (MPI-ESM) and investigate their effect on the biogeochemistry during the last deglaciation. Our results show that during the deglaciation, most of the terrestrial organic matter inputs to the ocean occurs during Meltwater Pulse 1a (between 15–14 ka) which leads to the transfer of 21.2 <span class=inline-formula>Gt C</span> of terrestrial carbon (mostly originating from wood and humus) to the ocean. Although this additional organic matter input is relatively small in comparison to the global ocean inventory (0.06 %) and thus does not have an impact on the global <span class=inline-formula>CO₂</span> flux, the terrestrial organic matter fluxes initiate oceanic outgassing in regional hotspots like in Indonesia for a few hundred years. Finally, sensitivity experiments highlight that terrestrial organic matter fluxes are the drivers of oceanic outgassing in flooded coastal regions during Meltwater Pulse 1a. Furthermore, the magnitude of outgassing is rather insensitive to higher carbon-to-nutrient ratios of the terrestrial organic matter. Our results provide a first estimate of the importance of terrestrial organic matter fluxes in a transient deglaciation simulation. Moreover, our model development is an important step towards a fully coupled carbon cycle in an Earth system model applicable to simulations at glacial–interglacial cycles." @default.
• W3199264342 created "2021-09-27" @default.
• W3199264342 creator A5034367423 @default.
• W3199264342 date "2021-09-10" @default.
• W3199264342 modified "2023-09-25" @default.
• W3199264342 title "Reply on CC1" @default.
• W3199264342 doi "https://doi.org/10.5194/cp-2021-112-ac1" @default.
• W3199264342 hasPublicationYear "2021" @default.
• W3199264342 type Work @default.
• W3199264342 sameAs 3199264342 @default.
• W3199264342 citedByCount "0" @default.
• W3199264342 crossrefType "peer-review" @default.
• W3199264342 hasAuthorship W3199264342A5034367423 @default.
• W3199264342 hasBestOaLocation W31992643421 @default.
• W3199264342 hasConcept C110872660 @default.
• W3199264342 hasConcept C111368507 @default.
• W3199264342 hasConcept C114793014 @default.
• W3199264342 hasConcept C127313418 @default.
• W3199264342 hasConcept C130309983 @default.
• W3199264342 hasConcept C140345934 @default.
• W3199264342 hasConcept C153294291 @default.
• W3199264342 hasConcept C15739521 @default.
• W3199264342 hasConcept C178790620 @default.
• W3199264342 hasConcept C180705331 @default.
• W3199264342 hasConcept C185592680 @default.
• W3199264342 hasConcept C18903297 @default.
• W3199264342 hasConcept C205649164 @default.
• W3199264342 hasConcept C207318512 @default.
• W3199264342 hasConcept C39432304 @default.
• W3199264342 hasConcept C48743137 @default.
• W3199264342 hasConcept C65440619 @default.
• W3199264342 hasConcept C6939412 @default.
• W3199264342 hasConcept C86803240 @default.
• W3199264342 hasConcept C91586092 @default.
• W3199264342 hasConceptScore W3199264342C110872660 @default.
• W3199264342 hasConceptScore W3199264342C111368507 @default.
• W3199264342 hasConceptScore W3199264342C114793014 @default.
• W3199264342 hasConceptScore W3199264342C127313418 @default.
• W3199264342 hasConceptScore W3199264342C130309983 @default.
• W3199264342 hasConceptScore W3199264342C140345934 @default.
• W3199264342 hasConceptScore W3199264342C153294291 @default.
• W3199264342 hasConceptScore W3199264342C15739521 @default.
• W3199264342 hasConceptScore W3199264342C178790620 @default.
• W3199264342 hasConceptScore W3199264342C180705331 @default.
• W3199264342 hasConceptScore W3199264342C185592680 @default.
• W3199264342 hasConceptScore W3199264342C18903297 @default.
• W3199264342 hasConceptScore W3199264342C205649164 @default.
• W3199264342 hasConceptScore W3199264342C207318512 @default.
• W3199264342 hasConceptScore W3199264342C39432304 @default.
• W3199264342 hasConceptScore W3199264342C48743137 @default.
• W3199264342 hasConceptScore W3199264342C65440619 @default.
• W3199264342 hasConceptScore W3199264342C6939412 @default.
• W3199264342 hasConceptScore W3199264342C86803240 @default.
• W3199264342 hasConceptScore W3199264342C91586092 @default.
• W3199264342 hasLocation W31992643421 @default.
• W3199264342 hasOpenAccess W3199264342 @default.
• W3199264342 hasPrimaryLocation W31992643421 @default.
• W3199264342 hasRelatedWork W156295062 @default.
• W3199264342 hasRelatedWork W2000285297 @default.
• W3199264342 hasRelatedWork W2001069665 @default.
• W3199264342 hasRelatedWork W2059105456 @default.
• W3199264342 hasRelatedWork W2107787376 @default.
• W3199264342 hasRelatedWork W2162457813 @default.
• W3199264342 hasRelatedWork W2170961021 @default.
• W3199264342 hasRelatedWork W4321495324 @default.
• W3199264342 hasRelatedWork W2001259875 @default.
• W3199264342 hasRelatedWork W2467781583 @default.
• W3199264342 isParatext "false" @default.
• W3199264342 isRetracted "false" @default.
• W3199264342 magId "3199264342" @default.
• W3199264342 workType "peer-review" @default.