Reanalysis of multi-temporal aerial images of Storglaciaren, Sweden (1959-99) - Part 1: Determination of length, area, and volume changes

被引:98
作者
Koblet, T. [1 ]
Gartner-Roer, I. [1 ]
Zemp, M. [1 ]
Jansson, P. [2 ]
Thee, P. [3 ]
Haeberli, W. [1 ]
Holmlund, P. [2 ]
机构
[1] Univ Zurich, Dept Geog, CH-8057 Zurich, Switzerland
[2] Dept Phys Geog & Quaternary Geol, S-10691 Stockholm, Sweden
[3] Swiss Fed Inst Forest Snow & Landscape Res, CH-8903 Birmensdorf, Switzerland
关键词
MASS-BALANCE RECORD; COLD SURFACE-LAYER; GLACIER; TEMPERATURE; MODEL; ACCURACY; ERROR; MAPS;
D O I
10.5194/tc-4-333-2010
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Storglaciaren, located in the Kebnekaise massif in northern Sweden, has a long history of glaciological research. Early photo documentations date back to the late 19th century. Measurements of front position variations and distributed mass balance have been carried out since 1910 and 1945/46, respectively. In addition to these in-situ measurements, aerial photographs have been taken at decadal intervals since the beginning of the mass balance monitoring program and were used to produce topographic glacier maps. Inaccuracies in the maps were a challenge to early attempts to derive glacier volume changes and resulted in major differences when compared to the direct glaciological mass balances. In this study, we reanalyzed dia-positives of the original aerial photographs of 1959, -69, -80, -90 and -99 based on consistent photogrammetric processing. From the resulting digital elevation models and orthophotos, changes in length, area, and volume of Storglaciaren were computed between the survey years, including an assessment of related errors. Between 1959 and 1999, Storglaciaren lost an ice volume of 19x10(6) m(3), which corresponds to a cumulative ice thickness loss of 5.69 m and a mean annual loss of 0.14 m. This ice loss resulted largely from a strong volume loss during the period 1959-80 and was partly compensated during the period 1980-99. As a consequence, the glacier shows a strong retreat in the 1960s, a slowing in the 1970s, and pseudo-stationary conditions in the 1980s and 1990s.
引用
收藏
页码:333 / 343
页数:11
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