Seasonal evolution of meltwater generation, storage and discharge at a non-temperate glacier in Svalbard
In glacierized catchments, meteorological inputs driving surface melting are translated into runoff outputs mediated by the glacier hydrological system: analysis of the relationship between meteorology and diurnal and seasonal patterns of runoff should reflect the functioning of that system, with th...
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| Format: | Default Article |
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2001
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| Online Access: | https://hdl.handle.net/2134/3326 |
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