FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3010176637> ?p ?o ?g. }

• W3010176637 endingPage "3110" @default.
• W3010176637 startingPage "3097" @default.
• W3010176637 abstract "Abstract. Mass loss from the Antarctic Ice Sheet constitutes the largest uncertainty in projections of future sea level rise. Ocean-driven melting underneath the floating ice shelves and subsequent acceleration of the inland ice streams are the major reasons for currently observed mass loss from Antarctica and are expected to become more important in the future. Here we show that for projections of future mass loss from the Antarctic Ice Sheet, it is essential (1) to better constrain the sensitivity of sub-shelf melt rates to ocean warming and (2) to include the historic trajectory of the ice sheet. In particular, we find that while the ice sheet response in simulations using the Parallel Ice Sheet Model is comparable to the median response of models in three Antarctic Ice Sheet Intercomparison projects – initMIP, LARMIP-2 and ISMIP6 – conducted with a range of ice sheet models, the projected 21st century sea level contribution differs significantly depending on these two factors. For the highest emission scenario RCP8.5, this leads to projected ice loss ranging from 1.4 to 4.0 cm of sea level equivalent in simulations in which ISMIP6 ocean forcing drives the PICO ocean box model where parameter tuning leads to a comparably low sub-shelf melt sensitivity and in which no surface forcing is applied. This is opposed to a likely range of 9.1 to 35.8 cm using the exact same initial setup, but emulated from the LARMIP-2 experiments with a higher melt sensitivity, even though both projects use forcing from climate models and melt rates are calibrated with previous oceanographic studies. Furthermore, using two initial states, one with a previous historic simulation from 1850 to 2014 and one starting from a steady state, we show that while differences between the ice sheet configurations in 2015 seem marginal at first sight, the historic simulation increases the susceptibility of the ice sheet to ocean warming, thereby increasing mass loss from 2015 to 2100 by 5 % to 50 %. Hindcasting past ice sheet changes with numerical models would thus provide valuable tools to better constrain projections. Our results emphasize that the uncertainty that arises from the forcing is of the same order of magnitude as the ice dynamic response for future sea level projections." @default.
• W3010176637 created "2020-03-13" @default.
• W3010176637 creator A5031563368 @default.
• W3010176637 creator A5035561950 @default.
• W3010176637 creator A5041611398 @default.
• W3010176637 creator A5048909931 @default.
• W3010176637 creator A5078036722 @default.
• W3010176637 date "2020-09-17" @default.
• W3010176637 modified "2023-10-16" @default.
• W3010176637 title "The role of history and strength of the oceanic forcing in sea level projections from Antarctica with the Parallel Ice Sheet Model" @default.
• W3010176637 cites W1541597243 @default.
• W3010176637 cites W1971799755 @default.
• W3010176637 cites W1985217958 @default.
• W3010176637 cites W1990701514 @default.
• W3010176637 cites W1993091516 @default.
• W3010176637 cites W2003371436 @default.
• W3010176637 cites W2010657574 @default.
• W3010176637 cites W2017552944 @default.
• W3010176637 cites W2017900025 @default.
• W3010176637 cites W2024966118 @default.
• W3010176637 cites W2049458304 @default.
• W3010176637 cites W2057500304 @default.
• W3010176637 cites W2057660933 @default.
• W3010176637 cites W2058268742 @default.
• W3010176637 cites W2062474226 @default.
• W3010176637 cites W2064260672 @default.
• W3010176637 cites W2072667640 @default.
• W3010176637 cites W2072844010 @default.
• W3010176637 cites W2078844631 @default.
• W3010176637 cites W2084869045 @default.
• W3010176637 cites W2102213705 @default.
• W3010176637 cites W2110417015 @default.
• W3010176637 cites W2133855861 @default.
• W3010176637 cites W2145016426 @default.
• W3010176637 cites W2161075265 @default.
• W3010176637 cites W2169971095 @default.
• W3010176637 cites W2320249130 @default.
• W3010176637 cites W2400117161 @default.
• W3010176637 cites W2604603169 @default.
• W3010176637 cites W2605719690 @default.
• W3010176637 cites W2616101533 @default.
• W3010176637 cites W2732270144 @default.
• W3010176637 cites W2761635722 @default.
• W3010176637 cites W2774886872 @default.
• W3010176637 cites W2794669705 @default.
• W3010176637 cites W2795267151 @default.
• W3010176637 cites W2797863887 @default.
• W3010176637 cites W2801080873 @default.
• W3010176637 cites W2887838553 @default.
• W3010176637 cites W2901463946 @default.
• W3010176637 cites W2907900190 @default.
• W3010176637 cites W2910997769 @default.
• W3010176637 cites W2911750130 @default.
• W3010176637 cites W2914023611 @default.
• W3010176637 cites W2915006888 @default.
• W3010176637 cites W2945377850 @default.
• W3010176637 cites W2946141553 @default.
• W3010176637 cites W2969316926 @default.
• W3010176637 cites W2995035319 @default.
• W3010176637 cites W3002630673 @default.
• W3010176637 cites W3004654262 @default.
• W3010176637 cites W3005758997 @default.
• W3010176637 cites W3043823404 @default.
• W3010176637 cites W4231500343 @default.
• W3010176637 cites W4240129602 @default.
• W3010176637 cites W81594258 @default.
• W3010176637 doi "https://doi.org/10.5194/tc-14-3097-2020" @default.
• W3010176637 hasPublicationYear "2020" @default.
• W3010176637 type Work @default.
• W3010176637 sameAs 3010176637 @default.
• W3010176637 citedByCount "11" @default.
• W3010176637 countsByYear W30101766372021 @default.
• W3010176637 countsByYear W30101766372022 @default.
• W3010176637 countsByYear W30101766372023 @default.
• W3010176637 crossrefType "journal-article" @default.
• W3010176637 hasAuthorship W3010176637A5031563368 @default.
• W3010176637 hasAuthorship W3010176637A5035561950 @default.
• W3010176637 hasAuthorship W3010176637A5041611398 @default.
• W3010176637 hasAuthorship W3010176637A5048909931 @default.
• W3010176637 hasAuthorship W3010176637A5078036722 @default.
• W3010176637 hasBestOaLocation W30101766371 @default.
• W3010176637 hasConcept C111368507 @default.
• W3010176637 hasConcept C114793014 @default.
• W3010176637 hasConcept C123750103 @default.
• W3010176637 hasConcept C127313418 @default.
• W3010176637 hasConcept C132651083 @default.
• W3010176637 hasConcept C134543767 @default.
• W3010176637 hasConcept C136894858 @default.
• W3010176637 hasConcept C146233495 @default.
• W3010176637 hasConcept C159985019 @default.
• W3010176637 hasConcept C192562407 @default.
• W3010176637 hasConcept C197115733 @default.
• W3010176637 hasConcept C197435368 @default.
• W3010176637 hasConcept C204323151 @default.
• W3010176637 hasConcept C2777093003 @default.
• W3010176637 hasConcept C2780223605 @default.
• W3010176637 hasConcept C39432304 @default.
• W3010176637 hasConcept C49204034 @default.

• next