FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2055866900> ?p ?o ?g. }

• W2055866900 endingPage "412" @default.
• W2055866900 startingPage "399" @default.
• W2055866900 abstract "Increased melting on glaciers and ice sheets and rising sea level are often mentioned as important aspects of the anticipated greenhouse warming of the earth's atmosphere. This paper deals with the sensitivity of Greenland's ice mass budget and presents a tentative projection of the Greenland component of future sea level rise for the next few hundred years. To do this, the ‘Villach II temperature scenario’ is prescribed,output from a comprehensive mass balance model is used to drive a high-resolution 3-D thermomechanic model of the ice sheet. The mass balance model consists of two parts: the accumulation part is based on presently observed values and is forced by changes in mean anr tempeerature. The ablation model is based on the degree-day method and accounts for daily and annual temperature cycle, a different degree-day factor for ice and snow melting and superimposed ice formation. Under present-day climatic conditions, the following total mass balance results (in ice equivalent per years): 599.3 × 109m3 of accumulation, 281.7 × 109m3 of runoff assuming a balanced budget, 317.6 × 109m3 of iceberg calving. A 1K uniform warming is then calculated to increase the runoff by 119.5 × 109m3. Since accumulation also increases by 32 × 109m3, this leads to reduction of the total mass balance by 887.5 × 109m3 of ice, corresponding to a sea level rise of 0.22 mm/yr. For temperature increase larger than 2.7 K, runoff, exceeds accumulation, and if ice sheet dynamics were to remain unchanged, this would add an extra amount of 0.8 mmyr to the worl's oceans. Imposing the Villach II scenario (warming up to 4.23 K) and accumulating mass balance changes forward in time (static response) would then result in a global sea level rise of 7.1 cm by 2100 AD, but this figure may go up to as much as 40 cm per century in case the warming is doubled. In a subsequent dynamic model involving the ice flow, the ice sheet is found to produce a counteracting effect by dynamically producing steeper slopes at the margin, thereby reducing the area over which runoff can take place. This effect is particularly apparent in the northeastern part of the ice sheet, and is also more pronounced for the smaller temperature perturbations. Nevertheless, all these experiments certainly highlight the vulnerability of the Greenland ice sheet with respect to a climatic warming." @default.
• W2055866900 created "2016-06-24" @default.
• W2055866900 creator A5073623680 @default.
• W2055866900 creator A5085961223 @default.
• W2055866900 creator A5091675030 @default.
• W2055866900 date "1991-03-01" @default.
• W2055866900 modified "2023-10-16" @default.
• W2055866900 title "The Greenland ice sheet and greenhouse warming" @default.
• W2055866900 cites W1583499505 @default.
• W2055866900 cites W1624104772 @default.
• W2055866900 cites W1637436322 @default.
• W2055866900 cites W1969578622 @default.
• W2055866900 cites W1981900098 @default.
• W2055866900 cites W2001579336 @default.
• W2055866900 cites W2006028711 @default.
• W2055866900 cites W2029353452 @default.
• W2055866900 cites W2031093546 @default.
• W2055866900 cites W2033556329 @default.
• W2055866900 cites W2071902319 @default.
• W2055866900 cites W2077517397 @default.
• W2055866900 cites W2141861302 @default.
• W2055866900 doi "https://doi.org/10.1016/0031-0182(91)90174-p" @default.
• W2055866900 hasPublicationYear "1991" @default.
• W2055866900 type Work @default.
• W2055866900 sameAs 2055866900 @default.
• W2055866900 citedByCount "153" @default.
• W2055866900 countsByYear W20558669002012 @default.
• W2055866900 countsByYear W20558669002013 @default.
• W2055866900 countsByYear W20558669002014 @default.
• W2055866900 countsByYear W20558669002015 @default.
• W2055866900 countsByYear W20558669002016 @default.
• W2055866900 countsByYear W20558669002017 @default.
• W2055866900 countsByYear W20558669002018 @default.
• W2055866900 countsByYear W20558669002020 @default.
• W2055866900 countsByYear W20558669002021 @default.
• W2055866900 countsByYear W20558669002023 @default.
• W2055866900 crossrefType "journal-article" @default.
• W2055866900 hasAuthorship W2055866900A5073623680 @default.
• W2055866900 hasAuthorship W2055866900A5085961223 @default.
• W2055866900 hasAuthorship W2055866900A5091675030 @default.
• W2055866900 hasBestOaLocation W20558669002 @default.
• W2055866900 hasConcept C100834320 @default.
• W2055866900 hasConcept C100970517 @default.
• W2055866900 hasConcept C111368507 @default.
• W2055866900 hasConcept C114793014 @default.
• W2055866900 hasConcept C123750103 @default.
• W2055866900 hasConcept C127045886 @default.
• W2055866900 hasConcept C127313418 @default.
• W2055866900 hasConcept C134543767 @default.
• W2055866900 hasConcept C136894858 @default.
• W2055866900 hasConcept C146233495 @default.
• W2055866900 hasConcept C18903297 @default.
• W2055866900 hasConcept C189059800 @default.
• W2055866900 hasConcept C197046000 @default.
• W2055866900 hasConcept C197435368 @default.
• W2055866900 hasConcept C205649164 @default.
• W2055866900 hasConcept C2780021526 @default.
• W2055866900 hasConcept C39432304 @default.
• W2055866900 hasConcept C49204034 @default.
• W2055866900 hasConcept C50477045 @default.
• W2055866900 hasConcept C81820708 @default.
• W2055866900 hasConcept C86803240 @default.
• W2055866900 hasConcept C91586092 @default.
• W2055866900 hasConceptScore W2055866900C100834320 @default.
• W2055866900 hasConceptScore W2055866900C100970517 @default.
• W2055866900 hasConceptScore W2055866900C111368507 @default.
• W2055866900 hasConceptScore W2055866900C114793014 @default.
• W2055866900 hasConceptScore W2055866900C123750103 @default.
• W2055866900 hasConceptScore W2055866900C127045886 @default.
• W2055866900 hasConceptScore W2055866900C127313418 @default.
• W2055866900 hasConceptScore W2055866900C134543767 @default.
• W2055866900 hasConceptScore W2055866900C136894858 @default.
• W2055866900 hasConceptScore W2055866900C146233495 @default.
• W2055866900 hasConceptScore W2055866900C18903297 @default.
• W2055866900 hasConceptScore W2055866900C189059800 @default.
• W2055866900 hasConceptScore W2055866900C197046000 @default.
• W2055866900 hasConceptScore W2055866900C197435368 @default.
• W2055866900 hasConceptScore W2055866900C205649164 @default.
• W2055866900 hasConceptScore W2055866900C2780021526 @default.
• W2055866900 hasConceptScore W2055866900C39432304 @default.
• W2055866900 hasConceptScore W2055866900C49204034 @default.
• W2055866900 hasConceptScore W2055866900C50477045 @default.
• W2055866900 hasConceptScore W2055866900C81820708 @default.
• W2055866900 hasConceptScore W2055866900C86803240 @default.
• W2055866900 hasConceptScore W2055866900C91586092 @default.
• W2055866900 hasIssue "4" @default.
• W2055866900 hasLocation W20558669001 @default.
• W2055866900 hasLocation W20558669002 @default.
• W2055866900 hasOpenAccess W2055866900 @default.
• W2055866900 hasPrimaryLocation W20558669001 @default.
• W2055866900 hasRelatedWork W1610309655 @default.
• W2055866900 hasRelatedWork W1967174588 @default.
• W2055866900 hasRelatedWork W2276037845 @default.
• W2055866900 hasRelatedWork W247331267 @default.
• W2055866900 hasRelatedWork W2968819518 @default.
• W2055866900 hasRelatedWork W3028106998 @default.
• W2055866900 hasRelatedWork W315636501 @default.
• W2055866900 hasRelatedWork W3210192027 @default.

• next