The SCE CDR was derived from a thorough reanalysis of NOAA satellite-derived maps of NH continental SCE, maps that date back to late 1966. We relied on comparisons between climatologies of the first 33 years of coarse-scale weekly NOAA maps and the most recent nine years of finer daily maps produced by NOAA, currently at the multi-agency National Ice Center. The reanalysis also benefited from a two-year overlap of the independently-produced daily and weekly products and the expertise of the Rutgers Global Snow Lab staff and colleagues elsewhere who were consulted throughout the project.
With this improved long-term satellite product we will document abrupt fluctuations of SCE on a variety of scales. This will include intra-seasonal variations within a snow season (such as described above), within season variability between Eurasia and North America and temporal trends associated with both. A preliminary assessment of associations of these results with large-scale atmospheric patterns (e.g. surface air temperature, mid-troposphere geopotential height) will be touched on here and discussed more fully in a companion paper at this meeting.