SNOP: Snow Physics
For the Snow Physics (SNOP) project, radar and aircraft data were presented in the form of case studies for three shoreline-parallel snow bands that occurred over lake Michigan. In all three cases a winter land breeze from one or both shores was shown to have an important role in organizing the low-level convergence and convective motions. These cases were compared with earlier studies of lake-effect snow bands on Lakes Erie and Ontario.
|Begin Date||1977-11-02 00:00:00|
|End Date||1977-12-16 23:59:59|
Maximum (North) Latitude:
Minimum (South) Latitude:
Minimum (West) Longitude: -87.826, Maximum (East) Longitude: -85.537