scholarly journals Relation between planimetric and volumetric measurements of permafrost coast erosion: a case study from Herschel Island, western Canadian Arctic

2016 ◽  
Vol 35 (1) ◽  
pp. 30313 ◽  
Author(s):  
Jaroslav Obu ◽  
Hugues Lantuit ◽  
Michael Fritz ◽  
Wayne H. Pollard ◽  
Torsten Sachs ◽  
...  
2016 ◽  
Vol 12 (1) ◽  
pp. 15-29 ◽  
Author(s):  
Lewis Archer ◽  
James D. Ford ◽  
Tristan Pearce ◽  
Slawomir Kowal ◽  
William A. Gough ◽  
...  

2019 ◽  
Vol 42 (2) ◽  
pp. 71-88 ◽  
Author(s):  
Pierre-Louis Têtu ◽  
Frédéric Lasserre ◽  
Sébastien Pelletier ◽  
Jackie Dawson

2001 ◽  
Vol 66 (3) ◽  
pp. 453-470 ◽  
Author(s):  
Peter C. Dawson

The semisubterranean whale-bone house is one of the most recognizable aspects of Thule Inuit culture. Following their arrival in the Canadian Arctic approximately 1,000 years ago, Thule peoples built these impressive and often enigmatic dwellings for occupation during the long winter months. Variability in the architectural properties of semisubterranean house forms has traditionally been used by archaeologists to infer cultural and historical relationships between regions, and establish seasonal and/or functional distinctions in usage. An analysis of 31 semisubterranean houses from two Thule winter village sites in the Canadian High Arctic using multivariate statistics and computer-aided drafting reveals a range of architectural variability that may represent attempts by Thule builders to accommodate 1) fluctuations in the availability of key building materials, 2) differences in household mobility, or 3) whaling-related social differentiation between households. These results have important implications for understanding the relationships among house form, environment, and culture in Thule Inuit society.


2006 ◽  
Vol 44 ◽  
pp. 329-338 ◽  
Author(s):  
Bea Alt ◽  
Katherine Wilson ◽  
Tom Carrières

AbstractThis case Study attempts to quantify the amount and timing of the import, export and through-flow of old ice in the Peary Channel–sverdrup Channel area of the northern Canadian Arctic Archipelago during the period 1998–2005. The Study combines quantitative weekly area-averaged ice coverage evaluations from the Canadian Ice Service (CIS) Digital Archive with detailed analysis of Radarsat imagery and ice-motion results from the CIS ice-motion algorithm. The results Show that in 1998 more than 70% of the old ice in Peary–sverdrup was lost, half by melt and export to the South and the other half by export north into the Arctic Ocean, and that no Arctic Ocean old ice was imported into Peary–sverdrup. A net import of 10% old ice was Seen in 1999, with Some indication of through-flow into Southern channels. In 2000, no net import of old ice occurred in Peary–sverdrup, but there was Significant through-flow, with evidence of old ice reaching the Northwest Passage by November. Full recovery of the old-ice regime was complete by the end of 2001. More than two-thirds of the recovery was due to the in Situ formation of Second-year ice. Conditions in the following 3 years were near normal.


2021 ◽  
Vol 764 ◽  
pp. 143861
Author(s):  
Dong-Young Back ◽  
Sun-Yong Ha ◽  
Brent Else ◽  
Mark Hanson ◽  
Samantha F. Jones ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document