Journal
JOURNAL OF GLACIOLOGY
Volume 58, Issue 211, Pages 941-952Publisher
INT GLACIOL SOC
DOI: 10.3189/2012JoG11J248
Keywords
-
Funding
- US National Science Foundation (NSF) grant [OPP-0821056]
- Natural Sciences and Engineering Research Council of Canada
- Canadian Polar Continental Shelf Program (Barnes Ice Cap field campaign)
- Environment Canada
- Centre National de la Recherche Scientifique (CNRS), France
- Institut Paul-Emile Victor (IPEV
- French Polar Institute)
- Programme International de Collaboration Scientifique (PICS) of CNRS
- Ministere des Relations Internationales du Quebec
- Ministere des Affaires Etrangeres et Europeennes de la Republique Francaise (Consulat General de France a Quebec) in the framework of the 63e Session de la Commission Permanente de Cooperation Franco-Quebecoise
Ask authors/readers for more resources
Snow grain-size characterization, its vertical and temporal evolution is a key parameter for the improvement and validation of snow and radiative transfer models (optical and microwave) as well as for remote-sensing retrieval methods. We describe two optical methods, one active and one passive shortwave infrared, for field determination of the specific surface area (SSA) of snow grains. We present a new shortwave infrared (SWIR) camera approach. This new method is compared with a SWIR laser-based system measuring snow albedo with an integrating sphere (Infra Red Integrating Sphere (IRIS)). Good accuracy (10%) and reproducibility in SSA measurements are obtained using the IRIS system on snow samples having densities greater than 200 kg m(-3), validated against X-ray microtomography measurements. The SWIRcam approach shows improved sensitivity to snow SSA when compared to a near-infrared camera, giving a better contrast of the snow stratigraphy in a snow pit.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available