气候变化领域集成服务门户(CCPortal): Ice-shelf damming in the glacial Arctic Ocean: Dynamical regimes of a basin-covering kilometre-thick ice shelf

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DOI	10.5194/tc-11-1745-2017
	Ice-shelf damming in the glacial Arctic Ocean: Dynamical regimes of a basin-covering kilometre-thick ice shelf
	Nilsson J.; Jakobsson M.; Borstad C.; Kirchner N.; Björk G.; Pierrehumbert R.T.; Stranne C.
发表日期	2017
ISSN	19940416
卷号	11 期号:4
英文摘要	Recent geological and geophysical data suggest that a 1ĝ€km thick ice shelf extended over the glacial Arctic Ocean during Marine Isotope Stage 6, about 140ĝ€000 years ago. Here, we theoretically analyse the development and equilibrium features of such an ice shelf, using scaling analyses and a one-dimensional ice-sheet–ice-shelf model. We find that the dynamically most consistent scenario is an ice shelf with a nearly uniform thickness that covers the entire Arctic Ocean. Further, the ice shelf has two regions with distinctly different dynamics: a vast interior region covering the central Arctic Ocean and an exit region towards the Fram Strait. In the interior region, which is effectively dammed by the Fram Strait constriction, there are strong back stresses and the mean ice-shelf thickness is controlled primarily by the horizontally integrated mass balance. A narrow transition zone is found near the continental grounding line, in which the ice-shelf thickness decreases offshore and approaches the mean basin thickness. If the surface accumulation and mass flow from the continental ice masses are sufficiently large, the ice-shelf thickness grows to the point where the ice shelf grounds on the Lomonosov Ridge. As this occurs, the back stress increases in the Amerasian Basin and the ice-shelf thickness becomes larger there than in the Eurasian Basin towards the Fram Strait. Using a one-dimensional ice-dynamic model, the stability of equilibrium ice-shelf configurations without and with grounding on the Lomonosov Ridge are examined. We find that the grounded ice-shelf configuration should be stable if the two Lomonosov Ridge grounding lines are located on the opposites sides of the ridge crest, implying that the downstream grounding line is located on a downward sloping bed. This result shares similarities with the classical result on marine ice-sheet stability of Weertman, but due to interactions between the Amerasian and Eurasian ice-shelf segments the mass flux at the downstream grounding line decreases rather than increases with ice thickness. © Author(s) 2017.
学科领域	glacier mass balance; grounding line; ice mechanics; ice sheet; ice shelf; ice thickness; marine isotope stage; sea ice; snow accumulation; transition zone; Amerasian Basin; Arctic; Arctic Ocean; Eurasian Basin; Fram Strait; Lomonosov Ridge
语种	英语
scopus关键词	glacier mass balance; grounding line; ice mechanics; ice sheet; ice shelf; ice thickness; marine isotope stage; sea ice; snow accumulation; transition zone; Amerasian Basin; Arctic; Arctic Ocean; Eurasian Basin; Fram Strait; Lomonosov Ridge
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/119365
作者单位	Department of Meteorology, Stockholm University, Stockholm, Sweden; Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden; Department of Geological Sciences, Stockholm University, Stockholm, Sweden; Department of Arctic Geophysics, University Centre in Svalbard, Longyearbyen, Norway; Department of Physical Geography, Stockholm University, Stockholm, Sweden; Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden; Department of Physics, University of Oxford, Oxford, United Kingdom
推荐引用方式 GB/T 7714	Nilsson J.,Jakobsson M.,Borstad C.,et al. Ice-shelf damming in the glacial Arctic Ocean: Dynamical regimes of a basin-covering kilometre-thick ice shelf[J],2017,11(4).
APA	Nilsson J..,Jakobsson M..,Borstad C..,Kirchner N..,Björk G..,...&Stranne C..(2017).Ice-shelf damming in the glacial Arctic Ocean: Dynamical regimes of a basin-covering kilometre-thick ice shelf.Cryosphere,11(4).
MLA	Nilsson J.,et al."Ice-shelf damming in the glacial Arctic Ocean: Dynamical regimes of a basin-covering kilometre-thick ice shelf".Cryosphere 11.4(2017).