globalchange  > 影响、适应和脆弱性
DOI: 10.5194/tc-8-2031-2014
Scopus记录号: 2-s2.0-84908661168
论文题名:
Fluctuations of a Greenlandic tidewater glacier driven by changes in atmospheric forcing: Observations and modelling of Kangiata Nunaata Sermia, 1859-present
作者: Lea J; M; , Mair D; W; F; , Nick F; M; , Rea B; R; , Van As D; , Morlighem M; , Nienow P; W; , Weidick A
刊名: Cryosphere
ISSN: 19940416
出版年: 2014
卷: 8, 期:6
起始页码: 2031
结束页码: 2045
语种: 英语
英文关键词: air temperature ; atmospheric forcing ; glacier dynamics ; Little Ice Age ; model validation ; tidewater glacier ; timescale ; Arctic ; Greenland
英文摘要: Many tidewater glaciers in Greenland are known to have undergone significant retreat during the last century following their Little Ice Age maxima. Where it is possible to reconstruct glacier change over this period, they provide excellent records for comparison to climate records, as well as calibration/validation for numerical models. These glacier change records therefore allow for tests of numerical models that seek to simulate tidewater glacier behaviour over multi-decadal to centennial timescales. Here we present a detailed record of behaviour from Kangiata Nunaata Sermia (KNS), SW Greenland, between 1859 and 2012, and compare it against available oceanographic and atmospheric temperature data between 1871 and 2012. We also use these records to evaluate the ability of a well-established one-dimensional flow-band model to replicate behaviour for the observation period. The record of terminus change demonstrates that KNS has advanced/retreated in phase with atmosphere and ocean climate anomalies averaged over multi-annual to decadal timescales. Results from an ensemble of model runs demonstrate that observed dynamics can be replicated. Model runs that provide a reasonable match to observations always require a significant atmospheric forcing component, but do not necessarily require an oceanic forcing component. Although the importance of oceanic forcing cannot be discounted, these results demonstrate that changes in atmospheric forcing are likely to be a primary driver of the terminus fluctuations of KNS from 1859 to 2012. We propose that the detail and length of the record presented makes KNS an ideal site for model validation exercises investigating links between climate, calving rates, and tidewater glacier dynamics.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/74769
Appears in Collections:影响、适应和脆弱性
气候变化与战略

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作者单位: Department of Geography and the Environment, University of Aberdeen, Elphinstone Road, Aberdeen, United Kingdom; University Centre in Svalbard (UNIS), P.O. Box 156, Longyearbyen, Norway; Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark; Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark; University of California, Irvine, Department of Earth System Science, Croul Hall, Irvine, CA, United States; Department of Geography, University of Edinburgh, Drummond Street, Edinburgh, United Kingdom; Department of Geography and Quaternary Geology, Stockholm University, Stockholm, Sweden

Recommended Citation:
Lea J,M,, Mair D,et al. Fluctuations of a Greenlandic tidewater glacier driven by changes in atmospheric forcing: Observations and modelling of Kangiata Nunaata Sermia, 1859-present[J]. Cryosphere,2014-01-01,8(6)
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