期刊论文详细信息
Polar research
Response of Eyjafjallajökull, Torfajökull and Tindfjallajökull ice caps in Iceland to regional warming, deduced by remote sensing
Etienne Berthier1  Finnur Pálsson2  Magnús Tumi Gudmundsson2  Thórdís Högnadóttir2  Helgi Björnsson2  Eyjólfur Magnússon2  Sverrir Gudmundsson3  Jørgen Dall4 
[1] Centre National de la Recherche Scientifique, Université de Toulouse, Laboratoire d'Etudes en Géophysique et Océanographie Spatiale Université de Toulouse 14 Avenue Edouard BelinToulouse, FR-31400, France;Institute of Earth Sciences, University of Iceland Sturlugata 7Askja, Reykjavík, IS-101, Iceland;Institute of Earth Sciences, University of Iceland Sturlugata 7Askja, Reykjavík, IS-101, Iceland Correspondence;National Space Institute, Technical University of DenmarkLyngby, DK-2800, Denmark
关键词: Remote sensing;    glacier mass balance;    regional warming;    Eyjafjallajökull;    Torfajökull;    Tindfjallajökull.;   
DOI  :  10.3402/polar.v30i0.7282
学科分类:自然科学(综合)
来源: Co-Action Publishing
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【 摘 要 】

We assess the volume change and mass balance of three ice caps in southern Iceland for two periods, 1979–1984 to 1998 and 1998 to 2004, by comparing digital elevation models (DEMs). The ice caps are Eyjafjallajökull (ca. 81 km2), Tindfjallajökull (ca. 15 km2) and Torfajökull (ca. 14 km2). The DEMs were compiled using aerial photographs from 1979 to 1984, airborne Synthetic Aperture Radar (SAR) images obtained in 1998 and two image pairs from the SPOT 5 satellite's high-resolution stereoscopic (HRS) instrument acquired in 2004. The ice-free part of the accurate DEM from 1998 was used as a reference map for co-registration and correction of the vertical offset of the other DEMs. The average specific mass balance was estimated from the mean elevation difference between glaciated areas of the DEMs. The glacier mass balance declined significantly between the two periods: from −0.2 to 0.2 m yr−1 w. eq. during the earlier period (1980s through 1998) to −1.8 to −1.5 m yr−1 w. eq. for the more recent period (1998–...

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CC BY-NC   

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