DOI: 10.5194/tc-9-1535-2015
Scopus记录号: 2-s2.0-84938811458
论文题名: Area, elevation and mass changes of the two southernmost ice caps of the Canadian Arctic Archipelago between 1952 and 2014
作者: Papasodoro C ; , Berthier E ; , Royer A ; , Zdanowicz C ; , Langlois A
刊名: Cryosphere
ISSN: 19940416
出版年: 2015
卷: 9, 期: 4 起始页码: 1535
结束页码: 1550
语种: 英语
英文关键词: airborne survey
; data set
; elevation
; historical record
; ice cap
; ice mechanics
; in situ measurement
; mass balance
; Pleiades
; satellite imagery
; snow water equivalent
; spatiotemporal analysis
; warming
; Baffin Island
; Canada
; Canadian Arctic
; Hudson Strait
; Nunavut
英文摘要: Grinnell and Terra Nivea Ice Caps are located on the southern Baffin Island, Nunavut, in the Canadian Arctic Archipelago. These relatively small ice caps have received little attention compared to the much larger ice masses further north. Their evolution can, however, give valuable information about the impact of the recent Arctic warming at lower latitudes (i.e. ∼ 62.5° N). In this paper, we measure or estimate historical and recent changes of area, elevation and mass of both ice caps using in situ, airborne and spaceborne data sets, including imagery from the Pléiades satellites. The area of Terra Nivea Ice Cap has decreased by 34 % since the late 1950s, while that of Grinnell Ice Cap has decreased by 20 % since 1952. For both ice caps, the areal reduction accelerated at the beginning of the 21st century. The estimated glacier-wide mass balance was -0.37 ± 0.21 m a-1 water equivalent (w.e.) over Grinnell Ice Cap for the 1952-2014 period, and -0.47 ± 0.16 m a-1 w.e. over Terra Nivea Ice Cap for the 1958/59-2014 period. Terra Nivea Ice Cap has experienced an accelerated rate of mass loss of -1.77 ± 0.36 m a-1 w.e. between 2007 and 2014. This rate is 5.9 times as negative when compared to the 1958/59-2007 period (-0.30 ± 0.19 m a-1 w.e.) and 2 times as negative when compared to the mass balance of other glaciers in the southern parts of Baffin Island over the 2003-2009 period. A similar acceleration in mass loss is suspected for the Grinnell Ice Cap, given the calculated elevation changes and the proximity to Terra Nivea Ice Cap. The recent increase in mass loss rates for these two ice caps is linked to a strong near-surface regional warming and a lengthening of the melt season into the autumn that may be indirectly strengthened by a later freezing of sea ice in the Hudson Strait sector. On a methodological level, our study illustrates the strong potential of Pléiades satellite data to unlock the under-exploited archive of old aerial photographs. © Author(s) 2015. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75266
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: Centre d'Applications et de Recherches en Télédétection, Université de Sherbrooke, Sherbrooke, QC, Canada; Centre d'Études Nordiques, Québec City, QC, Canada; Laboratoire d'Etudes en Géophysique et Océanographie Spatiales, Centre National de la Recherche Scientifique (LEGOS - CNRS, UMR5566), Université de Toulouse, Toulouse, France; Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Recommended Citation:
Papasodoro C,, Berthier E,, Royer A,et al. Area, elevation and mass changes of the two southernmost ice caps of the Canadian Arctic Archipelago between 1952 and 2014[J]. Cryosphere,2015-01-01,9(4)