The search result changed since you submitted your search request. Documents might be displayed in a different sort order.
  • search hit 1 of 11
Back to Result List

initMIP-Antarctica

  • Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial conditions on ice sheet model simulations, however, is still unclear. To better understand this influence, an initial state intercomparison exercise (initMIP) has been developed to compare, evaluate, and improve initialization procedures and estimate their impact on century-scale simulations. initMlP is the first set of experiments of the Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6), which is the primary Coupled Model Intercomparison Project Phase 6 (CMIP6) activity focusing on the Greenland and Antarctic ice sheets. Following initMlP-Greenland, initMlP-Antarctica has been designed to explore uncertainties associated with model initialization and spin-up and to evaluate the impact of changes in external forcings. Starting from the state of the Antarctic ice sheet at the end of the initialization procedure, three forward experiments are eachIce sheet numerical modeling is an important tool to estimate the dynamic contribution of the Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial conditions on ice sheet model simulations, however, is still unclear. To better understand this influence, an initial state intercomparison exercise (initMIP) has been developed to compare, evaluate, and improve initialization procedures and estimate their impact on century-scale simulations. initMlP is the first set of experiments of the Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6), which is the primary Coupled Model Intercomparison Project Phase 6 (CMIP6) activity focusing on the Greenland and Antarctic ice sheets. Following initMlP-Greenland, initMlP-Antarctica has been designed to explore uncertainties associated with model initialization and spin-up and to evaluate the impact of changes in external forcings. Starting from the state of the Antarctic ice sheet at the end of the initialization procedure, three forward experiments are each run for 100 years: a control run, a run with a surface mass balance anomaly, and a run with a basal melting anomaly beneath floating ice. This study presents the results of initMlP-Antarctica from 25 simulations performed by 16 international modeling groups. The submitted results use different initial conditions and initialization methods, as well as ice flow model parameters and reference external forcings. We find a good agreement among model responses to the surface mass balance anomaly but large variations in responses to the basal melting anomaly. These variations can be attributed to differences in the extent of ice shelves and their upstream tributaries, the numerical treatment of grounding line, and the initial ocean conditions applied, suggesting that ongoing efforts to better represent ice shelves in continental-scale models should continue.show moreshow less

Export metadata

Additional Services

Search Google Scholar Statistics
Metadaten
Author details:Helene SeroussiORCiD, Sophie NowickiORCiD, Erika Simon, Ayako Abe-OuchiORCiD, Torsten AlbrechtORCiDGND, Julien Brondex, Stephen CornfordORCiD, Christophe Dumas, Fabien Gillet-Chaulet, Heiko GoelzerORCiD, Nicholas R. Golledge, Jonathan M. Gregory, Ralf GreveORCiD, Matthew J. Hoffman, Angelika Humbert, Philippe HuybrechtsORCiD, Thomas Kleiner, Eric Larourl, Gunter Leguy, William H. Lipscomb, Daniel LowryORCiD, Matthias Mengel, Mathieu MorlighemORCiD, Frank PattynORCiD, Anthony J. Payne, David Pollard, Stephen F. Price, Aurelien QuiquetORCiD, Thomas J. Reerink, Ronja ReeseORCiDGND, Christian B. Rodehacke, Nicole-Jeanne SchlegelORCiD, Andrew Shepherd, Sainan Sun, Johannes Sutter, Jonas Van Breedam, Roderik S. W. van de Wal, Ricarda WinkelmannORCiDGND, Tong Zhang
DOI:https://doi.org/10.5194/tc-13-1441-2019
ISSN:1994-0416
ISSN:1994-0424
Title of parent work (English):The Cryosphere : TC ; an interactive open access journal of the European Geosciences Union
Subtitle (English):an ice sheet model initialization experiment of ISMIP6
Publisher:Copernicus
Place of publishing:Göttingen
Publication type:Article
Language:English
Date of first publication:2019/05/14
Publication year:2019
Release date:2021/02/11
Volume:13
Issue:5
Number of pages:31
First page:1441
Last Page:1471
Funding institution:Climate and Cryosphere (CliC) project; World Climate Research Programme (WCRP); National Aeronautics and Space AdministrationNational Aeronautics & Space Administration (NASA) [80NM0018D0004]; NASA Cryospheric Science, Sea Level Change Team, and Modeling Analysis and Prediction Program; National Center for Atmospheric Research - National Science Foundation [1852977]; Japan Society for the Promotion of Science (JSPS) KAKENHIMinistry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI) [JP16H02224, JP17H06104, JP17H06323]; European Research Council under the European CommunityEuropean Research Council (ERC); Theme 6 Environment, NACLIM (North Atlantic Climate) project [308299]; Nordic Centers of Excellence eSTICC (eScience Tool for Investigating Climate Change at High Northern Latitudes) - Nordforsk [57001]; US Department of Energy Office of Science, Biological and Environmental Research and Advanced Scientific Computing Research programsUnited States Department of Energy (DOE); Office of Science of the US Department of EnergyUnited States Department of Energy (DOE) [DEAC02-05CH11231]; Ministry of Education, Culture and Science (OCW), in the Netherlands; German Federal Ministry of Education and Research (BMBF) as Research for Sustainability initiative (FONA)Federal Ministry of Education & Research (BMBF) [FKZ: 01LP1511B]; European Research CouncilEuropean Research Council (ERC) [339108]; French National Research Agency (ANR)French National Research Agency (ANR) [ANR-15-CE01-0005-01]; GENCI-CINES [2017-016066]; Froggy platform of the CIMENT infrastructure - Rhone-Alpes region [CPER07_13 CIRA]; OSUG@2020 laBex [ANR10 LABX56]; Equip@Meso project [ANR-10-EQPX-29-01]; Deutsche Forschungsgemeinschaft (DFG)German Research Foundation (DFG) [LE1448/6-1, LE1448/7-1]; DFGGerman Research Foundation (DFG) [WI 4556/4-1]; NASANational Aeronautics & Space Administration (NASA) [NNX17AG65G]; NSFNational Science Foundation (NSF) [PLR-1603799, PLR-1644277]; European Regional Development Fund (ERDF)European Union (EU); German Federal Ministry of Education and ResearchFederal Ministry of Education & Research (BMBF); Gauss Centre for Supercomputing/Leibniz Supercomputing Centre [pr94ga]; National Science Foundation, Office of Polar Programs (OPP)National Science Foundation (NSF) [1443229]; FRS-FNRS MEDRISM projectFonds de la Recherche Scientifique - FNRS; BELSPO MIMO project (Stereo III); iceMOD project - Research Foundation - Flanders (FWO-Vlaanderen)FWO; Antarctica New Zealand Doctoral Scholarship program; New Zealand Ministry of Business, Innovation and EmploymentNew Zealand Ministry of Business, Innovation and Employment (MBIE) [15-VUW-131]
Organizational units:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Physik und Astronomie
DDC classification:5 Naturwissenschaften und Mathematik / 53 Physik / 530 Physik
Peer review:Referiert
Publishing method:Open Access / Gold Open-Access
DOAJ gelistet
License (German):License LogoCC-BY - Namensnennung 4.0 International
Accept ✔
This website uses technically necessary session cookies. By continuing to use the website, you agree to this. You can find our privacy policy here.