A two‐phase approach to the simulation of the combined isotope/salinity signal of marine ice
- 15 December 2001
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 106 (C12) , 31387-31401
- https://doi.org/10.1029/2000jc000207
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Significant marine-ice accumulation in the ablation zone beneath an Antarctic ice shelfJournal of Glaciology, 2001
- Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysisJournal of Glaciology, 2000
- Modeling the effects of frazil ice crystals on the dynamics and thermodynamics of Ice Shelf Water plumesJournal of Geophysical Research: Oceans, 1995
- Microstructure and electrical properties of marine ice and its relationship to meteoric ice and sea iceJournal of Geophysical Research: Oceans, 1994
- Evidence for basal marine ice in the Filchner–Ronne ice shelfNature, 1992
- Ice composition evidence of marine ice transfer along the bottom of a small Antarctic Ice ShelfGeophysical Research Letters, 1991
- Deuterium concentration and growth rate of Antarctic first‐year sea iceGeophysical Research Letters, 1988
- Freezing rate determination by the isotopic composition of the iceGeophysical Research Letters, 1987
- Oxygen Isotope Evidence for Bottom Freezing on the Amery Ice ShelfNature, 1972
- Hydrogen and oxygen isotope fractionation between ice and waterThe Journal of Physical Chemistry, 1968