Estimation and calibration of the water isotope differential diffusion length in ice core records
Palaeoclimatic information can be retrieved from the diffusion of the stable water isotope signal during firnification of snow. The diffusion length, a measure for the amount of diffusion a layer has experienced, depends on the firn temperature and the accumulation rate. We s...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2015-08-01
|
| Series: | The Cryosphere |
| Online Access: | http://www.the-cryosphere.net/9/1601/2015/tc-9-1601-2015.pdf |