Accelerated contributions of Canada's Baffin and Bylot Island glaciers to sea level rise over the past half century

被引:54
作者
Gardner, A. [1 ,2 ]
Moholdt, G. [3 ]
Arendt, A. [4 ]
Wouters, B. [5 ]
机构
[1] Clark Univ, Clark Grad Sch Geog, Worcester, MA 01610 USA
[2] Univ Michigan, Dept Atmospher Ocean & Space Sci, Ann Arbor, MI 48109 USA
[3] Univ Calif San Diego, Scripps Inst Oceanog, Inst Geophys & Planetary Phys, La Jolla, CA 92093 USA
[4] Univ Alaska, Inst Geophys, Fairbanks, AK 99775 USA
[5] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands
基金
加拿大自然科学与工程研究理事会;
关键词
BARNES-ICE-CAP; INCREASED MASS-LOSS; ELEVATION CHANGES; ACCURACY ASSESSMENT; ARCTIC ARCHIPELAGO; LASER ALTIMETRY; BALANCE; SURFACE; GRACE; SHEET;
D O I
10.5194/tc-6-1103-2012
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Canadian Arctic glaciers have recently contributed large volumes of meltwater to the world's oceans. To place recently observed glacier wastage into a historical perspective and to determine the region's longer-term (similar to 50 years) contribution to sea level, we estimate mass and volume changes for the glaciers of Baffin and Bylot Islands using digital elevation models generated from airborne and satellite stereoscopic imagery and elevation postings from repeat airborne and satellite laser altimetry. In addition, we update existing glacier mass change records from GRACE satellite gravimetry to cover the period from 2003 to 2011. Using this integrated approach, we find that the rate of mass loss from the region's glaciers increased from 11.1 +/- 3.4 Gt a(-1) (271 +/- 84 kg m(-2) a(-1)) for the period 1963-2006 to 23.8 +/- 6.1 Gt a-1 (581 +/- 149 kgm(-2) a(-1)) for the period 2003-2011. The doubling of the rate of mass loss is attributed to higher temperatures in summer with little change in annual precipitation. Through both direct and indirect effects, changes in summer temperatures accounted for 70-98% of the variance in the rate of mass loss, to which the Barnes Ice Cap was found to be 1.7 times more sensitive than either the Penny Ice Cap or the region's glaciers as a whole. This heightened sensitivity is the result of a glacier hypsometry that is skewed to lower elevations, which are shown to have a higher mass change sensitive to temperature compared to glacier surfaces at higher elevations. Between 2003 and 2011 the glaciers of Baffin and Bylot Islands contributed 0.07 +/- 0.02 mma(-1) to sea level rise accounting for 16% of the total contribution from glaciers outside of Green-land and Antarctica, a rate much higher than the longer-term average of 0.03 +/- 0.01 mma(-1) (1963 to 2006).
引用
收藏
页码:1103 / 1125
页数:23
相关论文
共 68 条
[1]   Elevation changes of ice caps in the Canadian Arctic Archipelago [J].
Abdalati, W ;
Krabill, W ;
Frederick, E ;
Manizade, S ;
Martin, C ;
Sonntag, J ;
Swift, R ;
Thomas, R ;
Yungel, J ;
Koerner, R .
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2004, 109 (F4)
[2]  
Andrews J. T., 2002, 1386J1 USGS, pJ162
[3]  
Bader H., 1954, J GLACIOL, V2, P319, DOI [10.3189/s0022143000025144, 10.3189/S0022143000025144, DOI 10.3189/S0022143000025144]
[4]   THE BAFFIN ISLAND EXPEDITION, 1950 [J].
Baird, P. D. .
GEOGRAPHICAL JOURNAL, 1952, 118 :267-279
[5]   Accuracy Assessment of Canadian Digital Elevation Data using ICESat [J].
Beaulieu, Alexandre ;
Clavet, Daniel .
PHOTOGRAMMETRIC ENGINEERING AND REMOTE SENSING, 2009, 75 (01) :81-86
[6]   Contribution of Alaskan glaciers to sea-level rise derived from satellite imagery [J].
Berthier, E. ;
Schiefer, E. ;
Clarke, G. K. C. ;
Menounos, B. ;
Remy, F. .
NATURE GEOSCIENCE, 2010, 3 (02) :92-95
[7]  
Bettadpur S, 2007, CSR LEVEL 2 PROCESSI, P327
[8]   INITIATION AND DEVELOPMENT OF THE LAURENTIDE AND CORDILLERAN ICE SHEETS FOLLOWING THE LAST INTERGLACIATION [J].
CLARK, PU ;
CLAGUE, JJ ;
CURRY, BB ;
DREIMANIS, A ;
HICOCK, SR ;
MILLER, GH ;
BERGER, GW ;
EYLES, N ;
LAMOTHE, M ;
MILLER, BB ;
MOTT, RJ ;
OLDALE, RN ;
STEA, RR ;
SZABO, JP ;
THORLEIFSON, LH ;
VINCENT, JS .
QUATERNARY SCIENCE REVIEWS, 1993, 12 (02) :79-114
[9]  
Dowdeswell EK, 2007, ARCT ANTARCT ALP RES, V39, P402, DOI 10.1657/1523-0430(05-123)[DOWDESWELL]2.0.CO
[10]  
2