气候变化领域集成服务门户(CCPortal): Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100

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DOI	10.5194/tc-14-1245-2020
	Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100
	Alevropoulos-Borrill A.V.; Nias I.J.; Payne A.J.; Golledge N.R.; Bingham R.J.
发表日期	2020
ISSN	19940416
起始页码	1245
结束页码	1258
卷号	14 期号:4
英文摘要	The response of ice streams in the Amundsen Sea Embayment (ASE) to future climate forcing is highly uncertain. Here we present projections of 21st century response of ASE ice streams to modelled local ocean temperature change using a subset of Coupled Model Intercomparison Project (CMIP5) simulations. We use the BISICLES adaptive mesh refinement (AMR) ice sheet model, with high-resolution grounding line resolving capabilities, to explore grounding line migration in response to projected sub-ice-shelf basal melting. We find a contribution to sea level rise of between 2.0 and 4.5 cm by 2100 under RCP8.5 conditions from the CMIP5 subset, where the mass loss response is linearly related to the mean ocean temperature anomaly. To account for uncertainty associated with model initialization, we perform three further sets of CMIP5-forced experiments using different parameterizations that explore perturbations to the prescription of initial basal melt, the basal traction coefficient and the ice stiffening factor. We find that the response of the ASE to ocean temperature forcing is highly dependent on the parameter fields obtained in the initialization procedure, where the sensitivity of the ASE ice streams to the sub-ice-shelf melt forcing is dependent on the choice of parameter set. Accounting for ice sheet model parameter uncertainty results in a projected range in sea level equivalent contribution from the ASE of between -0.02 and 12.1 cm by the end of the 21st century. . © 2020 Royal Society of Chemistry. All rights reserved.
英文关键词	catchment; climate forcing; CMIP; grounding line; ice sheet; sea level change; sea surface temperature; spatiotemporal analysis; temperature anomaly; Amundsen Sea; Antarctica; Southern Ocean; West Antarctica
语种	英语
来源期刊	Cryosphere
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/202012
作者单位	Centre for Polar Observation and Modelling, School of Geographical Sciences, University of Bristol, University Road, Bristol, BS8 1SS, United Kingdom; Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, United States; Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, United States; Antarctic Research Centre, Victoria University of Wellington, Wellington, New Zealand
推荐引用方式 GB/T 7714	Alevropoulos-Borrill A.V.,Nias I.J.,Payne A.J.,et al. Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100[J],2020,14(4).
APA	Alevropoulos-Borrill A.V.,Nias I.J.,Payne A.J.,Golledge N.R.,&Bingham R.J..(2020).Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100.Cryosphere,14(4).
MLA	Alevropoulos-Borrill A.V.,et al."Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100".Cryosphere 14.4(2020).