Modelling the late Holocene and future evolution of Monacobreen, northern Spitsbergen
Monacobreen is a 40 km long surge-type tidewater glacier in northern Spitsbergen. During 1991–1997 Monacobreen surged and advanced by about 2 km, but the front did not reach the maximum Little Ice Age (LIA) stand. Since 1997 the glacier front is retreating at a fast rate ( ∼125 m a −1 ). The questio...
| Published in: | The Cryosphere |
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| Format: | Text |
| Language: | English |
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2018
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| Online Access: | https://doi.org/10.5194/tc-12-3001-2018 https://tc.copernicus.org/articles/12/3001/2018/ |