FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022258134> ?p ?o ?g. }

• W2022258134 endingPage "55" @default.
• W2022258134 startingPage "37" @default.
• W2022258134 abstract "The variations of Northern Hemisphere continental ice sheet extent (excepting on Greenland) are simulated over the last glacial-interglacial cycle of Late Pleistocene time using an ice sheet model (ISM) which is asynchronously coupled to a climate model. The climate component of the coupled system consists of a global, two-dimensional, one level seasonal energy balance model (EBM) which includes seasonal ice feedback. The ice sheet component consists of a vertically integrated ice flow model which depends on latitude, longitude and time. Ice volume simulations obtained with the incorporation of the seasonal ice albedo feedback in the EBM (referred to as nonlinear EBM; NLEBM) have similar characteristics as those of an EBM in which the albedo is assumed independent of temperature (referred to as LEBM). It is also found that the full glacial Northern Hemisphere ice sheets predicted by the model exhibit a large sensitivity to orbital configuration and to variations in the solar constant. Although ice sheets are “easily” nucleated in the model, the North-American complex is shown to exhibit only weak sensitivity to variable solar forcing over the last glacial-interglacial cycle and no deglaciation is predicted to occur following the last glacial maximum. The Eurasian ice sheet on the other hand, exhibits a considerably greater sensitivity to orbital forcing, due to the higher continentality of Eurasia although no complete deglaciation is predicted by the model in this region either. Experiments with the NLEBM/ISM lead to the conclusion that the variations of other important geophysical variables such as atmospheric CO2 and changes in the thermohaline circulation of the ocean should be included in the climate modelling of the ice ages." @default.
• W2022258134 created "2016-06-24" @default.
• W2022258134 creator A5011271742 @default.
• W2022258134 creator A5072440155 @default.
• W2022258134 creator A5080313267 @default.
• W2022258134 date "1992-11-01" @default.
• W2022258134 modified "2023-09-23" @default.
• W2022258134 title "Simulations of continental ice sheet growth over the last glacial-interglacial cycle: experiments with a one level seasonal energy balance model including seasonal ice albedo feedback" @default.
• W2022258134 cites W126176336 @default.
• W2022258134 cites W1974361827 @default.
• W2022258134 cites W1974828561 @default.
• W2022258134 cites W1979383490 @default.
• W2022258134 cites W1980799929 @default.
• W2022258134 cites W1982297907 @default.
• W2022258134 cites W1982910644 @default.
• W2022258134 cites W1994274042 @default.
• W2022258134 cites W1994732436 @default.
• W2022258134 cites W2011732190 @default.
• W2022258134 cites W2018139159 @default.
• W2022258134 cites W2018956548 @default.
• W2022258134 cites W2022553189 @default.
• W2022258134 cites W2024795556 @default.
• W2022258134 cites W2026892947 @default.
• W2022258134 cites W2030083408 @default.
• W2022258134 cites W2043872181 @default.
• W2022258134 cites W2051175289 @default.
• W2022258134 cites W2053826541 @default.
• W2022258134 cites W2057236361 @default.
• W2022258134 cites W2064534700 @default.
• W2022258134 cites W2065433964 @default.
• W2022258134 cites W2071838648 @default.
• W2022258134 cites W2074430415 @default.
• W2022258134 cites W2076075458 @default.
• W2022258134 cites W2078721910 @default.
• W2022258134 cites W2079424523 @default.
• W2022258134 cites W2079739595 @default.
• W2022258134 cites W2093158629 @default.
• W2022258134 cites W2094394939 @default.
• W2022258134 cites W2108255545 @default.
• W2022258134 cites W2118222708 @default.
• W2022258134 cites W2121818196 @default.
• W2022258134 cites W2142614493 @default.
• W2022258134 cites W2147243326 @default.
• W2022258134 cites W2157426825 @default.
• W2022258134 cites W2172320674 @default.
• W2022258134 cites W4211014885 @default.
• W2022258134 cites W4231893887 @default.
• W2022258134 cites W4250993818 @default.
• W2022258134 doi "https://doi.org/10.1016/0921-8181(92)90021-2" @default.
• W2022258134 hasPublicationYear "1992" @default.
• W2022258134 type Work @default.
• W2022258134 sameAs 2022258134 @default.
• W2022258134 citedByCount "34" @default.
• W2022258134 countsByYear W20222581342012 @default.
• W2022258134 countsByYear W20222581342013 @default.
• W2022258134 countsByYear W20222581342014 @default.
• W2022258134 countsByYear W20222581342017 @default.
• W2022258134 crossrefType "journal-article" @default.
• W2022258134 hasAuthorship W2022258134A5011271742 @default.
• W2022258134 hasAuthorship W2022258134A5072440155 @default.
• W2022258134 hasAuthorship W2022258134A5080313267 @default.
• W2022258134 hasConcept C111368507 @default.
• W2022258134 hasConcept C114793014 @default.
• W2022258134 hasConcept C123750103 @default.
• W2022258134 hasConcept C127313418 @default.
• W2022258134 hasConcept C134543767 @default.
• W2022258134 hasConcept C136894858 @default.
• W2022258134 hasConcept C142362112 @default.
• W2022258134 hasConcept C149767477 @default.
• W2022258134 hasConcept C15739521 @default.
• W2022258134 hasConcept C180705331 @default.
• W2022258134 hasConcept C186240526 @default.
• W2022258134 hasConcept C189059800 @default.
• W2022258134 hasConcept C195886398 @default.
• W2022258134 hasConcept C197435368 @default.
• W2022258134 hasConcept C2778835443 @default.
• W2022258134 hasConcept C2780021526 @default.
• W2022258134 hasConcept C39996641 @default.
• W2022258134 hasConcept C49204034 @default.
• W2022258134 hasConcept C52119013 @default.
• W2022258134 hasConcept C554144382 @default.
• W2022258134 hasConcept C81027334 @default.
• W2022258134 hasConcept C81820708 @default.
• W2022258134 hasConcept C91586092 @default.
• W2022258134 hasConceptScore W2022258134C111368507 @default.
• W2022258134 hasConceptScore W2022258134C114793014 @default.
• W2022258134 hasConceptScore W2022258134C123750103 @default.
• W2022258134 hasConceptScore W2022258134C127313418 @default.
• W2022258134 hasConceptScore W2022258134C134543767 @default.
• W2022258134 hasConceptScore W2022258134C136894858 @default.
• W2022258134 hasConceptScore W2022258134C142362112 @default.
• W2022258134 hasConceptScore W2022258134C149767477 @default.
• W2022258134 hasConceptScore W2022258134C15739521 @default.
• W2022258134 hasConceptScore W2022258134C180705331 @default.
• W2022258134 hasConceptScore W2022258134C186240526 @default.
• W2022258134 hasConceptScore W2022258134C189059800 @default.
• W2022258134 hasConceptScore W2022258134C195886398 @default.
• W2022258134 hasConceptScore W2022258134C197435368 @default.

• next