SWEAT: Snow Water Equivalent with AlTimetry

• Main Authors: Unterberger, Manuela, Hardwick, Stephen, Agten, Dries, Benninga, Jan, Diaz Schümmer, Carlos, Donnerer, Julia, Fischer, Georg, Henriksen, Marie, Hippert-Ferrer, Alexandre, Jamali, Maryam, Marinaci, Stefano, Mould, Toby, Phelan, Liam, Rosker, Stephanie, Schrenker, Caroline, Schulze, Kerstin, Telo, Jorge, Monteiro, Bordalo
• Other Authors: Landbouw Economisch Instituut, Wageningen University and Research Wageningen (WUR), Laboratoire d'Informatique, Systèmes, Traitement de l'Information et de la Connaissance (LISTIC), Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )
• Format: Conference Object
• Language: English
• Published: HAL CCSD 2017
• Subjects: [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]; Sea ice
• Online Access: https://hal.archives-ouvertes.fr/hal-02184213; https://hal.archives-ouvertes.fr/hal-02184213/document; https://hal.archives-ouvertes.fr/hal-02184213/file/SWEAT.pdf

International audience Team Orange would like to thank FFG and ESA for organising the Summer School Alpbach 2016. Also thanks to all the tutors and lecturers guiding Team Orange towards this product, and a special thank to our team tutors. Abstract Snow Water Equivalent (SWE) is not directly measured by current satellite missions but has a significant impact on society and our lack of understanding contributes to significant inaccuracies in current estimations of hydrological and climate models, calculations of the Earth's energy balance (albedo) and flood predictions. To address this, the SWEAT (Snow Water Equivalent with AlTimetry) mission aims to measure SWE directly on sea ice and land in the polar regions above 60 • and below-60 • latitude. The primary scientific objectives are to (a) improve estimations of global SWE from passive microwave products and (b) improve numerical snow and climate models. The mission will implement a novel combination of Ka-and Ku-band radioaltimeter technology, each providing different snow penetration properties. Airborne Laser altimeter campaigns will shadow the satellite orbit path early, middle and late winter for the first two years of the mission to confirm Ka-Band surface measurement accuracies. The combined difference in signal penetration results will enable more accurate determination of SWE.Therefore, the SWEAT mission aims to improve estimations of global SWE interpreted from passive microwave products, and improve the reliability of numerical snow and climate models.