Evolution of a stream ecosystem in recently deglaciated terrain
Climate change and associated glacial recession create new stream habitat that leads to the assembly of new riverine communities through primary succession.
Brown, LE +5 more
core +1 more source
Ice dynamics at the mouth of ice stream B, Antarctica [PDF]
Robert Bindschadler +3 more
openalex +1 more source
A Coupled Marine Ice-Stream – Ice-Shelf Model [PDF]
Isabelle Muszynski, G. E. Birchfield
openalex +1 more source
Water-pressure Coupling of Sliding and Bed Deformation: III. Application to Ice Stream B, Antarctica [PDF]
Richard B. Alley +3 more
openalex +1 more source
Microearthquakes Under and Alongside Ice Stream B, Antarctica. Detected By A New Passive Seismic Array [PDF]
Donald D. Blankenship +3 more
openalex +1 more source
Late glacial dynamics on the continental shelf of NE-Greenland - implications from submarine landforms [PDF]
Favorable sea-ice conditions gave way to an acoustic survey offshore NE-Greenland in 2009. The acquired data set clearly depicts an area of sediment ridges in an area of at app. 18 x 9 km. The ridges are found in water depths between 270 and 350 m.
Jensen, Laura +3 more
core
Surface Features of Ice Stream B, Marie Byrd Land, West Antarctica [PDF]
Patricia Vornberger, I. M. Whillans
openalex +1 more source
Flow of Rutford Ice Stream and Comparison with Carlson Inlet, Antarctica [PDF]
R. M. Frolich +2 more
openalex +1 more source
An overview of STIP interval 18: September 1985, the G-Z encounter [PDF]
The primary period of interest during September 1985 is the few days surrounding the ICE encounter with comet Giacobini-Zinner(G-Z) which occurred at 1102 UT on 11 September.
Zwickl, R. D.
core +1 more source
Enlargement of the active rift during glaciations [PDF]
During the last glaciation, an ice sheet covered Iceland approximately 1000 m thick. A reconstruction of the ice flow lines shows that the ice sheet was partly drained through fast-flowing streams.
Bourgeois, Olivier +2 more
core +1 more source

