Paper No. JAWRA-10-0126-P of the Journal of the American Water Resources Association (JAWRA). Discussions are open until six months from print publication.
Glacier Variability (1967-2006) in the Teton Range, Wyoming, United States1
Version of Record online: 21 OCT 2011
© 2011 American Water Resources Association
JAWRA Journal of the American Water Resources Association
Volume 48, Issue 1, pages 187–196, February 2012
How to Cite
Edmunds, J., Tootle, G., Kerr, G., Sivanpillai, R. and Pochop, L. (2012), Glacier Variability (1967-2006) in the Teton Range, Wyoming, United States. JAWRA Journal of the American Water Resources Association, 48: 187–196. doi: 10.1111/j.1752-1688.2011.00607.x
- Issue online: 1 FEB 2012
- Version of Record online: 21 OCT 2011
- Received July 31, 2010; accepted August 9, 2011.
- Teton Range;
Edmunds, Jake, Glenn Tootle, Greg Kerr, Ramesh Sivanpillai, and Larry Pochop, 2011. Glacier Variability (1967-2006) in the Teton Range, Wyoming, United States. Journal of the American Water Resources Association (JAWRA) 48(1): 187-196. DOI: 10.1111/j.1752-1688.2011.00607.x
Abstract: Glacier area and volume changes were quantified through the use of historical aerial photographs in Wyoming’s Teton Range. Glacier area changes in the Teton Range were estimated for three glaciers using unrectified aerial photography from 1967 to 2006. The total surface area of the three glaciers was 0.53 km2 in 1967 and 0.40 km2 in 2006, a decrease of 25% during the 39-year period. The smallest glacier, Teepe, experienced the greatest area loss (60 ± 3%), whereas the largest glacier, Teton Glacier, lost 17 ± 3% of the 1967 area. For the current research, aerial photography from 1967 to 2002 was used to estimate glacier volume loss using stereoscopy techniques. The aerial photographs provide a finer resolution when compared with other datasets including satellite imagery (e.g., Landsat). Volume loss for the three glaciers was estimated to be 3.20 ± 0.46 million cubic meters over the period of 1967 to 2002. In assessing the primary climatic driver of the glacier ice loss, observed summer (June, July, and August) temperature data showed a statistically significant increase in temperatures when comparing the period of study (1968 to 2006) with historical temperatures from 1911 to 1967. When comparing spring (April 1st Snow Water Equivalent) snowpack for the period of study with historical records beginning in 1931, a significant difference in snowpack was not observed.