Surface energy balance and modelled firn density at four sites of the accumulation area of the Greenland ice sheet
Recent Arctic atmospheric warming induces more frequent surface melt in the accumulation area of the Greenland ice sheet. This increased melting modifies the near-surface firn structure and density and may reduce the firn’s capacity to retain meltwater. Yet, few long-term observational records are a...
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Arctic Data Center
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Online Access: | https://search.dataone.org/view/urn:uuid:f015f8b7-82f4-4ea8-b7a0-304f442da0cc |