Improvement of Polar Snow Microwave Brightness Temperature Simulations for Dense Wind Slab and Large Grain
Author:
Affiliation:
1. Département de géomatique appliquée, Université de Sherbrooke, Sherbrooke, QC, Canada
2. Centre d’études nordiques, Québec, QC, Canada
3. Institut des géosciences de l’environnement, Université Grenoble Alpes, Grenoble, France
Funder
Natural Sciences and Engineering Research Council
Fonds de Recherche du Québec - Nature et technologie
Canadian Fund for Innovation
Environment and Climate Change Canada
Polar Knowledge Canada
Publisher
Institute of Electrical and Electronics Engineers (IEEE)
Link
http://xplorestaging.ieee.org/ielx8/36/10354519/10608056.pdf?arnumber=10608056
Reference40 articles.
1. Remote sensing of snow with passive microwave radiometers—A review of current algorithms;Amlien,2008
2. Measurement of vertical profiles of snow specific surface area with a 1 cm resolution using infrared reflectance: instrument description and validation
3. Best Practices in Crafting the Calibrated, Enhanced-Resolution Passive-Microwave EASE-Grid 2.0 Brightness Temperature Earth System Data Record
4. Physical properties of Arctic versus subarctic snow: Implications for high latitude passive microwave snow water equivalent retrievals
5. Development of the Terrestrial Snow Mass Mission
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