A groove-ploughing theory for the production of mega-scale glacial lineations, and implications for ice-stream mechanics.
(2003)
Journal Article
Clark, C., Tulaczyk, M., Stokes, C., & Canals, M. (2003). A groove-ploughing theory for the production of mega-scale glacial lineations, and implications for ice-stream mechanics. Journal of Glaciology, 49(165), 240-256
Outputs (5)
Giant glacial grooves detected on Landsat ETM+ satellite imagery (2003)
Journal Article
Stokes, C., & Clark, C. (2003). Giant glacial grooves detected on Landsat ETM+ satellite imagery. International Journal of Remote Sensing, 24(5), 905-910. https://doi.org/10.1080/01431160110115069
The Dubawnt Lake palaeo-ice stream: evidence for dynamic ice sheet behaviour on the Canadian Shield and insights regarding the controls on ice-stream location and vigour. (2003)
Journal Article
Stokes, C., & Clark, C. (2003). The Dubawnt Lake palaeo-ice stream: evidence for dynamic ice sheet behaviour on the Canadian Shield and insights regarding the controls on ice-stream location and vigour
Researchers Discuss Abrupt Climate Change: Ice Sheets and Oceans in Action. (2003)
Journal Article
Dokken, T., Andrews, J., Hemming, S., Stokes, C., & Jansen, E. (2003). Researchers Discuss Abrupt Climate Change: Ice Sheets and Oceans in Action. Eos, Transactions American Geophysical Union, 84(20), 189-193
Laurentide ice streaming on the Canadian Shield: A conflict with the soft-bedded ice stream paradigm? (2003)
Journal Article
Stokes, C., & Clark, C. (2003). Laurentide ice streaming on the Canadian Shield: A conflict with the soft-bedded ice stream paradigm?. Geology, 31(4), 347-350. https://doi.org/10.1130/0091-7613%282003%29031%3C0347%3Alisotc%3E2.0.co%3B2Elucidating the controls on the location and vigor of ice streams is crucial to understanding the processes that lead to fast disintegration of ice flows and ice sheets. In the former North American Laurentide ice sheet, ice stream occurrence appears... Read More about Laurentide ice streaming on the Canadian Shield: A conflict with the soft-bedded ice stream paradigm?.