Changes in area and geodetic mass balance of small glaciers, Polar Urals, Russia, 1950-2008

被引:22
|
作者
Shahgedanova, Maria [1 ,2 ]
Nosenko, Gennady [3 ]
Bushueva, Irina [3 ]
Ivanov, Mikhail [3 ]
机构
[1] Univ Reading, Dept Geog & Environm Sci, Reading, Berks, England
[2] Univ Reading, Walker Inst Climate Syst Res, Reading, Berks, England
[3] Russian Acad Sci, Inst Geog, Moscow, Russia
基金
俄罗斯基础研究基金会;
关键词
MULTITEMPORAL AERIAL IMAGES; EASTERN SIBERIA; SWEDEN; 1959-99; NATIONAL-PARK; REANALYSIS; MOUNTAINS; NORWAY; VOLUME; STORGLACIAREN; JOTUNHEIMEN;
D O I
10.3189/2012JoG11J233
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Changes in area of 30 small glaciers (mostly <1 km(2)) in the northern Polar Urals (67.5 - 68.25 degrees N) between 1953 and 2000 were assessed using historic aerial photography from 1953 and 1960, ASTER and panchromatic Landsat ETM+ imagery from 2000, and data from 1981 and 2008 terrestrial surveys. Changes in volume and geodetic mass balance of IGAN and Obruchev glaciers were calculated using data from terrestrial surveys in 1963 and 2008. In total, glacier area declined by 22.3 +/- 3.9% in the 1953/60-2000 period. The areas of individual glaciers decreased by 4-46%. Surfaces of Obruchev and IGAN glaciers lowered by 22.5 +/- 1.7 m and 14.9 +/- 2.1 m. Over 45 years, geodetic mass balances of Obruchev and IGAN glaciers were -20.66 +/- 2.91 and -13.54 +/- 2.57 m w.e. respectively. Glacier shrinkage in the Polar Urals is related to a summer warming of 1 C between 1953-81 and 1981-2008 and its rates are consistent with other regions of northern Asia but are higher than in Scandinavia. While glacier shrinkage intensified in the 1981-2000 period relative to 1953-81, increasing winter precipitation and shading effects slowed glacier wastage in 2000-08.
引用
收藏
页码:953 / 964
页数:12
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