DOI: 10.5194/tc-15-3329-2021
论文题名: Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea
作者: Hillebrand T.R. ; Stone J.O. ; Koutnik M. ; King C. ; Conway H. ; Hall B. ; Nichols K. ; Goehring B. ; Gillespie M.K.
刊名: Cryosphere
ISSN: 19940416
出版年: 2021
卷: 15, 期: 7 起始页码: 3329
结束页码: 3354
语种: 英语
英文关键词: glacial deposit
; glacier dynamics
; glacier retreat
; grounding line
; Holocene
; ice sheet
; ice thickness
; last deglaciation
; Antarctica
; Beardmore Glacier
; Darwin Glacier
; East Antarctica
; Hatherton Glacier
; Minna
; Niger [Nigeria]
; Nigeria
; Ross Island
; Ross Sea
; Southern Ocean
; Transantarctic Mountains
英文摘要: Chronologies of glacier deposits in the Transantarctic Mountains provide important constraints on grounding-line retreat during the last deglaciation in the Ross Sea. However, between Beardmore Glacier and Ross Island - a distance of some 600km - the existing chronologies are generally sparse and far from the modern grounding line, leaving the past dynamics of this vast region largely unconstrained. We present exposure ages of glacial deposits at three locations alongside the Darwin-Hatherton Glacier System - including within 10km of the modern grounding line - that record several hundred meters of Late Pleistocene to Early Holocene thickening relative to present. As the ice sheet grounding line in the Ross Sea retreated, Hatherton Glacier thinned steadily from about 9 until about 3ka. Our data are equivocal about the maximum thickness and Mid-Holocene to Early Holocene history at the mouth of Darwin Glacier, allowing for two conflicting deglaciation scenarios: (1) ĝ1/4500m of thinning from 9 to 3ka, similar to Hatherton Glacier, or (2) ĝ1/4950m of thinning, with a rapid pulse of ĝ1/4600m thinning at around 5ka. We test these two scenarios using a 1.5-dimensional flowband model, forced by ice thickness changes at the mouth of Darwin Glacier and evaluated by fit to the chronology of deposits at Hatherton Glacier. The constraints from Hatherton Glacier are consistent with the interpretation that the mouth of Darwin Glacier thinned steadily by ĝ1/4500m from 9 to 3ka. Rapid pulses of thinning at the mouth of Darwin Glacier are ruled out by the data at Hatherton Glacier. This contrasts with some of the available records from the mouths of other outlet glaciers in the Transantarctic Mountains, many of which thinned by hundreds of meters over roughly a 1000-year period in the Early Holocene. The deglaciation histories of Darwin and Hatherton glaciers are best matched by a steady decrease in catchment area through the Holocene, suggesting that Byrd and/or Mulock glaciers may have captured roughly half of the catchment area of Darwin and Hatherton glaciers during the last deglaciation. An ensemble of three-dimensional ice sheet model simulations suggest that Darwin and Hatherton glaciers are strongly buttressed by convergent flow with ice from neighboring Byrd and Mulock glaciers, and by lateral drag past Minna Bluff, which could have led to a pattern of retreat distinct from other glaciers throughout the Transantarctic Mountains. © Copyright: Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/164708
Appears in Collections: 气候变化与战略
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作者单位: Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, United States; School of Earth and Climate Science and Climate Change Institute, University of Maine, Orono, ME 04469, United States; Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, United States; Faculty of Engineering and Science, Western Norway University of Applied Sciences, Sogndal, 6856, Norway; Fluid Dynamics and Solid Mechanics Group, Los Alamos National Laboratory, Los Alamos, NM 87545, United States
Recommended Citation:
Hillebrand T.R.,Stone J.O.,Koutnik M.,et al. Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea[J]. Cryosphere,2021-01-01,15(7)