Abstract
The gas enclosed in the ice of a temperatezone glacier, Storbreen in the Jotunheimen district of Norway, has been systematically examined (COACHMAN ET AL., 1956). In this study samples of ice were taken from the glacier surface in a longitudinal line from the fim area to the terminus. Ice thus sampled has both a gradient in age and a gradient in depth of passage in the glacier interior.
Cite
CITATION STYLE
APA
Coachman, L. K., Enns, T., & Scholander, P. F. (1958). Gas Loss from a Temperate Glacier. Tellus A: Dynamic Meteorology and Oceanography, 10(4), 493–495. https://doi.org/10.3402/tellusa.v10i4.9257
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.
Already have an account? Sign in
Sign up for free