Abstract
The microstructure and density of ice layers in snowpacks is poorly quantified. Here we present a new field method for measuring the density of ice layers caused by melt or rain-on-snow events. The method was used on 87 ice layer samples taken from natural and artificial ice layers in the Canadian Arctic and mid-latitudes. Mean measured ice layer density was 909 ± 28 kg m−3 with a standard deviation of 23 kg m−3, significantly higher than values typically used in the literature.
| Original language | English |
|---|---|
| Pages (from-to) | 2069-2074 |
| Number of pages | 6 |
| Journal | The Cryosphere |
| Volume | 10 |
| Issue number | 5 |
| DOIs | |
| Publication status | Published - 14 Sept 2016 |
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