Articles | Volume 10, issue 3
https://doi.org/10.5194/tc-10-1229-2016
https://doi.org/10.5194/tc-10-1229-2016
Research article
 | 
15 Jun 2016
Research article |  | 15 Jun 2016

Case study of spatial and temporal variability of snow cover, grain size, albedo and radiative forcing in the Sierra Nevada and Rocky Mountain snowpack derived from imaging spectroscopy

Felix C. Seidel, Karl Rittger, S. McKenzie Skiles, Noah P. Molotch, and Thomas H. Painter

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Felix C. Seidel on behalf of the Authors (12 Apr 2016)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (18 Apr 2016) by Florent Dominé
AR by Lorena Grabowski on behalf of the Authors (26 Apr 2016)  Author's response
ED: Publish as is (29 Apr 2016) by Florent Dominé
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Short summary
Quantifying the snow albedo effect is an important step to predict water availability as well as changes in climate and sea level. We use imaging spectroscopy to determine optical properties of mountain snow. We find an inverse relationship between snow albedo and grain size as well as between elevation and grain size. Under strong melt conditions, however, we show that the optical-equivalent snow grain size increases slower than expected at lower elevations and we explain possible reasons.