Abstract:ÌýA decline in theÌýnorthern hemisphere terrestrial seasonal snow extent has been observed fromÌýsatellite observations, especially in the springtime at highÌýlatitude. Snow mass or snow water equivalentÌý(SWE) is an importantÌývariable in the annual water budget of river catchments in cold regions,ÌýespeciallyÌýin places that rely on seasonal snowmelt runoff for waterÌýsupply. ÌýYet uncertainty persists in our ability toÌýquantify snowÌýmass from local to global scales using satellite observing instruments. ThisÌýpresentationÌýconsiders conceptual advances in theory that underpin applicationsÌýto map SWE from satellite passiveÌýmicrowave observations and illustrates howÌýprogress is now constrained by instrument characteristics. ItÌýthen discussesÌýhow recent field experiments to observe seasonal snow accumulation from radarÌýhaveÌýadvanced our knowledge even further to the point where radar systems nowÌýoffer a viable solution to localÌýmapping of SWE. Two possibilities to map SWEÌýhave emerged from this recent radar research, one thatÌýuses Ku-band backscatterÌýsignatures, and the other using radar interferometry. We focus on the first ofÌýthese two approaches, but recognize the opportunities for the second approach.ÌýThe challenge will be toÌýcombine different observation methods (including thoseÌýfrom airborne systems), to optimize the long-termÌýsatellite record of SWE,Ìýthereby providing significant insight into SWE climatology. Ìý
Bio:ÌýRichard Kelly received his PhD from the University of Bristol before becoming a Lecturer in Physical Geography at Birkbeck College, University of London, in 1994. In 2000 he was an Associate Research Scientist at NASA/GSFC & UMBC before joining the University of Waterloo, Canada in 2006, where he has been ever since. Along the way, he has been on the editorial board of IEEE JSTARS (past) and SPIE Journal of Applied Remote Sensing (current) and was the President of the Eastern Snow Conference. Recently he was theÌýAssociate Dean of Research in the Faculty of Environment at the University of Waterloo and he willÌýbe the Chair of the Department of Geography and Environmental Management from January 2017. His Research interests are concerned with the use of active and passive microwave remote sensing of snow and ice. He was the PI for the NASA AMSR-E snow product and currently leads the JAXA AMSR2 snow product team. He has conducted field research in Canada, USA, Finland, Norway, Switzerland, Pakistan and the UK. Currently is part of a team looking at rainwater harvesting in S. India in an era of climate change.