globalchange  > 过去全球变化的重建
DOI: 10.1007/s00382-012-1471-4
Scopus记录号: 2-s2.0-84878107636
论文题名:
Linear response functions to project contributions to future sea level
作者: Winkelmann R.; Levermann A.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2013
卷: 40, 期:2017-11-12
起始页码: 2579
结束页码: 2588
语种: 英语
英文关键词: Antarctica ; Greenland ; Response functions ; Sea-level rise ; Thermal expansion
英文摘要: We propose linear response functions to separately estimate the sea-level contributions of thermal expansion and solid ice discharge from Greenland and Antarctica. The response function formalism introduces a time-dependence which allows for future rates of sea-level rise to be influenced by past climate variations. We find that this time-dependence is of the same functional type, R(t) ∼ t α, for each of the three subsystems considered here. The validity of the approach is assessed by comparing the sea-level estimates obtained via the response functions to projections from comprehensive models. The pure vertical diffusion case in one dimension, corresponding to α=-0.5, is a valid approximation for thermal expansion within the ocean up to the middle of the twenty first century for all Representative Concentration Pathways. The approximation is significantly improved for α = - 0.7. For the solid ice discharge from Greenland we find an optimal value of α = -0.7. Different from earlier studies we conclude that solid ice discharge from Greenland due to dynamic thinning is bounded by 0.42 m sea-level equivalent. Ice discharge induced by surface warming on Antarctica is best captured by a positive value of α = 0.1 which reflects the fact that ice loss increases with the cumulative amount of heat available for softening the ice in our model. © 2012 Springer-Verlag.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/54907
Appears in Collections:过去全球变化的重建

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作者单位: Potsdam Institute for Climate Impact Research, Potsdam, Germany

Recommended Citation:
Winkelmann R.,Levermann A.. Linear response functions to project contributions to future sea level[J]. Climate Dynamics,2013-01-01,40(2017-11-12)
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