Briksdalsbreen in western Norway: AD 1900-2004 frontal fluctuations as a combined effect of variations in winter precipitation and summer temperature

@article{Nesje2005BriksdalsbreenIW,
  title={Briksdalsbreen in western Norway: AD 1900-2004 frontal fluctuations as a combined effect of variations in winter precipitation and summer temperature},
  author={Atle Nesje},
  journal={The Holocene},
  year={2005},
  volume={15},
  pages={1245 - 1252}
}
  • A. Nesje
  • Published 1 December 2005
  • Geology
  • The Holocene
Mountain glaciers and ice caps are sensitive to changes in regional and global climate. Temporal glacier variations, manifested in change of volume, area and length, provide some of the clearest signals of climate change in nature. Therefore, glaciers are considered key indicators for the detection of global warming. Except for a few glaciers in western Scandinavia, glaciers in Europe are in retreat, following the global trend. Maritime (coastal) glaciers in western Norway experienced positive… Expand

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