Similar Papers

Paper Title
Journal
Date
Author
Reconstructing the basal thermal regime of an ice stream in a landscape of selective linear erosion: Glen Avon, Cairngorm Mountains, Scotland
Adrian M Hall ... Neil F Glasser
Boreas | VOL. 32
Adrian M Hall, et. al.Adrian M Hall ... Neil F Glasser
01 Mar 2003
Thermal regime and dynamics of the West Antarctic ice sheet
Hermann Engelhardt
Annals of Glaciology | VOL. 39
Hermann EngelhardtHermann Engelhardt
01 Jan 2004
A landform-driven simulation of deglaciation of the Scandinavian Ice Sheet and the PalGlac project’s progress on data-modelling integration
Chris Clark ... Sarah Bradley
-
Chris Clark, et. al.Chris Clark ... Sarah Bradley
27 Nov 2024
The subglacial thermal organisation (STO) of ice sheets
Johan Kleman ... Neil F Glasser
Quaternary Science Reviews | VOL. 26
Johan Kleman, et. al.Johan Kleman ... Neil F Glasser
08 Feb 2007
View more papers

More From: Boreas

Paper Title
Journal
Date
Author
A synthesis of luminescence and 14C dated dust mass accumulation rates for loess‐palaeosol sequences from the Middle Danube Basin
Zoran M Perić ... Slobodan B Marković
Boreas | VOL. -
Zoran M Perić, et. al.Zoran M Perić ... Slobodan B Marković
24 Jan 2025
Geochronological investigations at the maximum extent of the Fennoscandian Ice Sheet during the Late Weichselian glaciation in northern Germany
Nikolas Krauß ... Michael Kenzler
Boreas | VOL. -
Nikolas Krauß, et. al.Nikolas Krauß ... Michael Kenzler
22 Jan 2025
An inventory of subglacial overdeepenings in southern Germany and Austria
Lukas Gegg ... Angela Landgraf
Boreas | VOL. -
Lukas Gegg, et. al.Lukas Gegg ... Angela Landgraf
16 Jan 2025
The impact of the structural framework of the North German Basin on Pleistocene tunnel‐valley formation
Jörg Lang ... Sonja Breuer
Boreas | VOL. -
Jörg Lang, et. al.Jörg Lang ... Sonja Breuer
16 Jan 2025
View more papers

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.