Crevasse ages on the northern margin of Ice Stream C, West Antarctica

Annals of Glaciology

Volumn 34, Issue , 2002, Pages 209-216

  Smith, B E ^a   Lord, N E ^a   Bentley, C R ^a  

^a UNIVERSITY OF WASHINGTON   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CREVASSE; GROUND PENETRATING RADAR; ICE STREAM;

ANTARCTICA;

EID: 0036333157     PISSN: 02603055     EISSN: None     Source Type: Journal    
DOI: 10.3189/172756402781817932     Document Type: Article

References (16)

1. A water-piracy hypothesis for the stagnation of Ice Stream C. Antarctica
2. Surface velocity and mass balance of Ice Streams D and E, West Antarctica
3. High-resolution radar on Ice Stream B2, Antarctica: Measurements of electromagnetic wave speed in firn and strain history from buried crevasses
4. The role of the margins in the dynamics of an active ice stream
5. Firm densification: an empirical model
6. Weak bands within Ice Stream B, West Antarctica
7. Tributaries of West Antarctic ice streams revealed by RADARSAT interferometry
8. Dielectric constant of heterogenous mixtures
9. Sub-surface crevasse formation on ice streams
10. Timing of stagnation of Ice Stream C. West Antarctica, from short-pulse radar studies of buried surface crevasses
11. Airborne-radar studies: Ice Streams A. B and C, West Antarctica
12. Spatial variability at shallow snow-layer depths in central Dronning Maud Land, East Antarctica
13. Development of enhanced ice flow at the southern margin of Ice Stream D, Antarctica
14. West Antarctic ice streams draining into the Ross Ice Shelf: Configuration and mass balance
15. Mass balance of Ice Stream B, West Antarctica