• Nie Znaleziono Wyników

Future evolution of the Greenland Ice Sheet in a coupled climate and ice sheet model: CESM2.1-CISM2.1 contribution to ISMIP6

N/A
N/A
Protected

Academic year: 2021

Share "Future evolution of the Greenland Ice Sheet in a coupled climate and ice sheet model: CESM2.1-CISM2.1 contribution to ISMIP6"

Copied!
2
0
0

Pełen tekst

(1)

Delft University of Technology

Future evolution of the Greenland Ice Sheet in a coupled climate and ice sheet model:

CESM2.1-CISM2.1 contribution to ISMIP6

Muntjewerf, Laura; Lipscomb, William; Thayer-Calder, Kate; Bradley, Sarah; Fyke, Jeremy; Ernani da Silva, Carolina; Sellevold, Raymond; Petrini, Michele; Vizcaino, Miren; More Authors

Publication date 2019

Document Version Final published version Citation (APA)

Muntjewerf, L., Lipscomb, W., Thayer-Calder, K., Bradley, S., Fyke, J., Ernani da Silva, C., Sellevold, R., Petrini, M., Vizcaino, M., & More Authors (2019). Future evolution of the Greenland Ice Sheet in a coupled climate and ice sheet model: CESM2.1-CISM2.1 contribution to ISMIP6. Poster session presented at EGU General Assembly 2019 , Vienna, Austria.

Important note

To cite this publication, please use the final published version (if applicable). Please check the document version above.

Copyright

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons. Takedown policy

Please contact us and provide details if you believe this document breaches copyrights. We will remove access to the work immediately and investigate your claim.

This work is downloaded from Delft University of Technology.

(2)

Geophysical Research Abstracts Vol. 21, EGU2019-16223-1, 2019 EGU General Assembly 2019

© Author(s) 2019. CC Attribution 4.0 license.

Future evolution of the Greenland Ice Sheet in a coupled climate and ice

sheet model: CESM2.1-CISM2.1 contribution to ISMIP6

Laura Muntjewerf (1), William Lipscomb (2), Kate Thayer-Calder (2), Bill Sacks (2), Sarah Bradley (1,6), Marcus Lofverstrom (3), Jeremy Fyke (4,5), Carolina Ernani da Silva (1), Raymond Sellevold (1), Michele Petrini (1), and Miren Vizcaino (1)

(1) Delft University of Technology, Netherlands (l.muntjewerf@tudelft.nl), (2) National Center for Atmospheric Research, USA, (6) University of Sheffield, UK, (3) University of Arizona, USA, (4) Associated Engineering Group Ltd., Canada, (5) Los Alamos National Laboratory, USA

There are large uncertainties in projections of 21st century and future multi-century global sea level rise. Part of the uncertainty stems from the lack of ability to robustly resolve interactions and feedbacks between ice sheets and the rest of the climate system in global circulation models. Coupling an ice sheet model to a global climate model will help us in this regard.

The Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6) is a CMIP6-endorsed MIP that focusses on the Greenland and Antarctic Ice Sheets. One ISMIP6 goal is a set of simulations with climate models coupled to ice sheet models (ISM). This will enable to assess the climatic impact of the ice sheet dynamic response onto the climate.

The Community Earth System Model version 2.1 (CESM2.1) includes a of bi-directional coupling with the Com-munity Ice Sheet Model (CISM2.1) over the Greenland Ice Sheet. With this model we can assess ice sheet and climate interactions at a previously unprecedented level of detail. Furthermore, routing of ice sheet meltwater and calving into the ocean, as well as adaptive ice sheet topography enables studies of the impact of a changing ice sheet on future atmospheric and ocean circulation patterns.

Here we present the CESM2.1-CISM2.1 simulations under ISMIP6 guidelines that have been analyzed to date. Four simulations will be carried out: 1) a pre-industrial control steady state simulation (piControl-withism), 2) a 500-year simulation with a 1% yr−1 increase CO2 up till the value of 4 times the pre-industrial concentration (1pctCO2to4x-withism), 3) a historical simulation 1850-2015 (historical-withism) and 4) a future evolution simu-lation following the emission scenario RCP8.5 and its extension to year 2,300 (ssp585-withism). In the analysis, we focus on key features of the global and polar climate: the time evolution of the North Atlantic Meridional Overturning Circulation strength (NAMOC), the Greenland surface albedo, surface melt and surface mass balance (SMB), and the dynamical ice sheet change and contribution to eustatic sea level rise.

Cytaty

Powiązane dokumenty

Obecnie w ystępują onii do Rady Adwokackiej o p rzenie­ sienie swych siedzib do Poznania, co stwarza dla Rady w ielk ie trudności. odbyło się plenarne posiedzenie

Prócz tego zamieszczono w niej przepisy o zaopatrzeniu emerytalnym z tytułu przejęcia na własność państwa przedsiębiorstw i gospodarstw rolnych oraz przepisy

Figure 6 shows the maximum support pressures calculated with the new blow-out model (Figure 4), Balthaus’s model (Figure 1) and Broere’s model (Figure 2) for the case of

Ciąża u kobiet z przewlekłą chorobą nerek stanowi wyzwanie, które należy rozpatrywać na kilku płasz- czyznach: wpływu przewlekłej choroby nerek na przebieg ciąży i

Feliks Kazimierz Terlikowski ogłosił przeszło 100 prac, przeważnie w języku polskim w Rocznikach Nauk Rolniczych.. Nie ma ani jednego tom u tego czasopisma, w

Zadaniem niniejszego opracowania jest ukazanie działań łódzkich władz terenowych oraz aparatu bezpieczeństwa wobec placówek oświatowo-wycho- wawczych: przedszkola i

C’est la communauté dans la souffrance que, après les Mais… de Zadig, le moi lyrique de Voltaire professe dans le Poème sur le désastre de Lisbonne : « Je respecte

Postępowy dziennik „La Espana” już 28 stycznia podkreślał narodowy aspekt powstania i walkę przeciwko despotyzmowi: „w Polsce się biją o sprawę, o