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Meteorological inventory of rain-on-snow events in the Canadian Arctic Archipelago and satellite detection assessment using passive microwave data
Authors:Caroline Dolant  A. Langlois  L. Brucker  A. Royer  A. Roy  B. Montpetit
Affiliation:1. Centre d’Applications et de Recherche en Télédétection, Université de Sherbrooke, Quebec, Canada;2. Centre for Northern Studies, Université Laval, Quebec, Canada;3. Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA;4. Goddard Earth Sciences Technology and Research Studies and Investigations, Universities Space Research Association, Columbia, MD, USA
Abstract:
The spatial and temporal distributions of rain-on-snow (ROS) events across the Canadian Arctic Archipelago (CAA) remain poorly understood owing to their sporadic nature in time and space. This situation motivated the development of remote sensing detection algorithms. This paper uses a large meteorological dataset across the CAA to adapt an existing ROS-detection algorithm developed in a previous study by our group. Results highlight the spatial distribution and evolution of ROS occurrences reported since 1985 at 14 weather stations across the CAA. Results show that >600 ROS events were inventoried since 1985, for which >70% were classified as pure rain (liquid form) and 30% as mixed precipitation (solid/liquid). Of the pure rain events, 75% occurred during spring, 14% during fall, 8% during summer and <1% during winter. Such events can have significant impacts on ungulate grazing conditions through the creation of ice layers, causing serious problems for caribou calf survival, especially during the migration period. This paper introduces an adaptation for larger scale Arctic application of a detection algorithm (sensitivity analysis on the detection threshold) with an error of ~5%. The validation, however, remains limited due to a short study period and limited number of sites.
Keywords:Rain-on-snow events  Canadian Arctic Archipelago (CAA)  climatological trends  microwave radiometry
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