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Professor Chris Stokes' Outputs (4)

Geodetic mass balance of Azarova glacier, Kodar mountains, eastern Siberia, and its links to observed and projected climatic change (2011)
Journal Article
Shahgenova, M., Popovnin, V., Aleynikov, A., & Stokes, C. (2011). Geodetic mass balance of Azarova glacier, Kodar mountains, eastern Siberia, and its links to observed and projected climatic change. Annals of Glaciology, 52(58), 129-137. https://doi.org/10.3189/172756411797252275

The Kodar mountains in eastern Siberia accommodate 30 small, cold-based glaciers with a combined surface area previously estimated at 19 km2. Very little is known about these glaciers, which were first surveyed in the late 1950s. In this paper, we us... Read More about Geodetic mass balance of Azarova glacier, Kodar mountains, eastern Siberia, and its links to observed and projected climatic change.

The composition and internal structure of drumlins: Complexity, commonality, and implications for a unifying theory of their formation (2011)
Journal Article
Stokes, C., Spagnolo, M., & Clark, C. (2011). The composition and internal structure of drumlins: Complexity, commonality, and implications for a unifying theory of their formation. Earth-Science Reviews, 107(3-4), 398-422. https://doi.org/10.1016/j.earscirev.2011.05.001

Investigation of drumlins is significant to both glaciology and palaeoglaciology but the sheer diversity of their composition and internal structure is often cited as a major obstacle towards a satisfactory (unifying?) explanation of their formation.... Read More about The composition and internal structure of drumlins: Complexity, commonality, and implications for a unifying theory of their formation.

Glacial geomorphology of the north-west sector of the Laurentide Ice Sheet (2011)
Journal Article
Brown, V., Stokes, C., & O'Cofaigh, C. (2011). Glacial geomorphology of the north-west sector of the Laurentide Ice Sheet. Journal of Maps, 2011, 409-428. https://doi.org/10.4113/jom.2011.1224

This paper presents a new map of the glacial geomorphology of $\sim$ 800,000 km\up{2} of north-west Canada. The mapped area includes parts of Northwest Territories and Nunavut which were covered by the Laurentide Ice Sheet during the Late Wisconsinan... Read More about Glacial geomorphology of the north-west sector of the Laurentide Ice Sheet.