FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2155012905> ?p ?o ?g. }

• W2155012905 endingPage "982" @default.
• W2155012905 startingPage "969" @default.
• W2155012905 abstract "Abstract. In the present work the Arctic sea ice in the mid-Holocene and the pre-industrial climates are analysed and compared on the basis of climate-model results from the Paleoclimate Modelling Intercomparison Project phase 2 (PMIP2) and phase 3 (PMIP3). The PMIP3 models generally simulate smaller and thinner sea-ice extents than the PMIP2 models both for the pre-industrial and the mid-Holocene climate. Further, the PMIP2 and PMIP3 models all simulate a smaller and thinner Arctic summer sea-ice cover in the mid-Holocene than in the pre-industrial control climate. The PMIP3 models also simulate thinner winter sea ice than the PMIP2 models. The winter sea-ice extent response, i.e. the difference between the mid-Holocene and the pre-industrial climate, varies among both PMIP2 and PMIP3 models. Approximately one half of the models simulate a decrease in winter sea-ice extent and one half simulates an increase. The model-mean summer sea-ice extent is 11 % (21 %) smaller in the mid-Holocene than in the pre-industrial climate simulations in the PMIP2 (PMIP3). In accordance with the simple model of Thorndike (1992), the sea-ice thickness response to the insolation change from the pre-industrial to the mid-Holocene is stronger in models with thicker ice in the pre-industrial climate simulation. Further, the analyses show that climate models for which the Arctic sea-ice responses to increasing atmospheric CO2 concentrations are similar may simulate rather different sea-ice responses to the change in solar forcing between the mid-Holocene and the pre-industrial. For two specific models, which are analysed in detail, this difference is found to be associated with differences in the simulated cloud fractions in the summer Arctic; in the model with a larger cloud fraction the effect of insolation change is muted. A sub-set of the mid-Holocene simulations in the PMIP ensemble exhibit open water off the north-eastern coast of Greenland in summer, which can provide a fetch for surface waves. This is in broad agreement with recent analyses of sea-ice proxies, indicating that beach-ridges formed on the north-eastern coast of Greenland during the early- to mid-Holocene." @default.
• W2155012905 created "2016-06-24" @default.
• W2155012905 creator A5004451314 @default.
• W2155012905 creator A5029621342 @default.
• W2155012905 creator A5029805389 @default.
• W2155012905 date "2013-04-15" @default.
• W2155012905 modified "2023-10-01" @default.
• W2155012905 title "The sensitivity of the Arctic sea ice to orbitally induced insolation changes: a study of the mid-Holocene Paleoclimate Modelling Intercomparison Project 2 and 3 simulations" @default.
• W2155012905 cites W1605282505 @default.
• W2155012905 cites W1627075293 @default.
• W2155012905 cites W1888180832 @default.
• W2155012905 cites W1930393311 @default.
• W2155012905 cites W1932364988 @default.
• W2155012905 cites W1971451183 @default.
• W2155012905 cites W1978912155 @default.
• W2155012905 cites W1981998039 @default.
• W2155012905 cites W1997120413 @default.
• W2155012905 cites W2000444336 @default.
• W2155012905 cites W2024417959 @default.
• W2155012905 cites W2049709446 @default.
• W2155012905 cites W2059603165 @default.
• W2155012905 cites W2060359957 @default.
• W2155012905 cites W2061291627 @default.
• W2155012905 cites W2066211400 @default.
• W2155012905 cites W2090761054 @default.
• W2155012905 cites W2101005049 @default.
• W2155012905 cites W2101863114 @default.
• W2155012905 cites W2112617203 @default.
• W2155012905 cites W2117298528 @default.
• W2155012905 cites W2124252360 @default.
• W2155012905 cites W2125600063 @default.
• W2155012905 cites W2142027333 @default.
• W2155012905 cites W2144096669 @default.
• W2155012905 cites W2147439389 @default.
• W2155012905 cites W2152320606 @default.
• W2155012905 cites W2154442841 @default.
• W2155012905 cites W2163832574 @default.
• W2155012905 cites W2492865770 @default.
• W2155012905 cites W3121683766 @default.
• W2155012905 doi "https://doi.org/10.5194/cp-9-969-2013" @default.
• W2155012905 hasPublicationYear "2013" @default.
• W2155012905 type Work @default.
• W2155012905 sameAs 2155012905 @default.
• W2155012905 citedByCount "20" @default.
• W2155012905 countsByYear W21550129052013 @default.
• W2155012905 countsByYear W21550129052014 @default.
• W2155012905 countsByYear W21550129052015 @default.
• W2155012905 countsByYear W21550129052016 @default.
• W2155012905 countsByYear W21550129052017 @default.
• W2155012905 countsByYear W21550129052020 @default.
• W2155012905 countsByYear W21550129052022 @default.
• W2155012905 crossrefType "journal-article" @default.
• W2155012905 hasAuthorship W2155012905A5004451314 @default.
• W2155012905 hasAuthorship W2155012905A5029621342 @default.
• W2155012905 hasAuthorship W2155012905A5029805389 @default.
• W2155012905 hasBestOaLocation W21550129051 @default.
• W2155012905 hasConcept C111368507 @default.
• W2155012905 hasConcept C117935615 @default.
• W2155012905 hasConcept C127313418 @default.
• W2155012905 hasConcept C132651083 @default.
• W2155012905 hasConcept C136894858 @default.
• W2155012905 hasConcept C140345934 @default.
• W2155012905 hasConcept C143510601 @default.
• W2155012905 hasConcept C161798024 @default.
• W2155012905 hasConcept C168754636 @default.
• W2155012905 hasConcept C196735533 @default.
• W2155012905 hasConcept C197435368 @default.
• W2155012905 hasConcept C33683781 @default.
• W2155012905 hasConcept C39432304 @default.
• W2155012905 hasConcept C49204034 @default.
• W2155012905 hasConcept C518008717 @default.
• W2155012905 hasConceptScore W2155012905C111368507 @default.
• W2155012905 hasConceptScore W2155012905C117935615 @default.
• W2155012905 hasConceptScore W2155012905C127313418 @default.
• W2155012905 hasConceptScore W2155012905C132651083 @default.
• W2155012905 hasConceptScore W2155012905C136894858 @default.
• W2155012905 hasConceptScore W2155012905C140345934 @default.
• W2155012905 hasConceptScore W2155012905C143510601 @default.
• W2155012905 hasConceptScore W2155012905C161798024 @default.
• W2155012905 hasConceptScore W2155012905C168754636 @default.
• W2155012905 hasConceptScore W2155012905C196735533 @default.
• W2155012905 hasConceptScore W2155012905C197435368 @default.
• W2155012905 hasConceptScore W2155012905C33683781 @default.
• W2155012905 hasConceptScore W2155012905C39432304 @default.
• W2155012905 hasConceptScore W2155012905C49204034 @default.
• W2155012905 hasConceptScore W2155012905C518008717 @default.
• W2155012905 hasIssue "2" @default.
• W2155012905 hasLocation W21550129051 @default.
• W2155012905 hasLocation W21550129052 @default.
• W2155012905 hasOpenAccess W2155012905 @default.
• W2155012905 hasPrimaryLocation W21550129051 @default.
• W2155012905 hasRelatedWork W1643456360 @default.
• W2155012905 hasRelatedWork W1981266108 @default.
• W2155012905 hasRelatedWork W2155012905 @default.
• W2155012905 hasRelatedWork W2525422358 @default.
• W2155012905 hasRelatedWork W2551285701 @default.
• W2155012905 hasRelatedWork W2992873450 @default.
• W2155012905 hasRelatedWork W3134792003 @default.

• next