On the relationship between δ O 2 ∕N 2 variability and ice sheet surface conditions in Antarctica
On the relationship between δ O 2 ∕N 2 variability and ice sheet surface conditions in Antarctica
About this item
Full title
Author / Creator
Journal title
Language
English
Formats
More information
Scope and Contents
Contents
While the processes controlling pore closure are broadly understood, the physical mechanisms driving the associated elemental fractionation remains ambiguous. Previous studies have shown that the pore closure process leads to a depletion in small-sized molecules (e.g. H2, O2, Ar, Ne, He) in ice core bubbles relative to larger-sized molecules like N...
Alternative Titles
Full title
On the relationship between δ O 2 ∕N 2 variability and ice sheet surface conditions in Antarctica
Authors, Artists and Contributors
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_crossref_primary_10_5194_tc_18_3741_2024
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_crossref_primary_10_5194_tc_18_3741_2024
Other Identifiers
ISSN
1994-0424
E-ISSN
1994-0424
DOI
10.5194/tc-18-3741-2024
