The Ross Sea Dipole - temperature, snow accumulation and sea ice variability in the Ross Sea region, Antarctica, over the past 2700 years (2018)
Attributed to:
Measuring and modelling the Raymond Effect for to infer low strain-rate ice rheology
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/cp-14-193-2018
Publication URI: http://dx.doi.org/10.5194/cp-14-193-2018
Type: Journal Article/Review
Parent Publication: Climate of the Past
Issue: 2
ISSN: 1814-9324