Ice temperatures measured in a grid of boreholes, Western Greenland, 2014-2016
Ice in the ablation zone of the Greenland ice sheet is known to contain vertical temperature gradients that arise from conduction at the boundaries, the addition of strain and latent heat, and advective heat transport. A three‐dimensional array of temperature measurements in a grid of boreholes reve...
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| Format: | Dataset |
| Language: | unknown |
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Arctic Data Center
2017
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| Online Access: | https://doi.org/10.18739/A26561 |