Snowfall in the Northern Great Lakes: Lessons Learned from a Multisensor Observatory

Author:

Kulie Mark S.1,Pettersen Claire2,Merrelli Aronne J.2,Wagner Timothy J.2,Wood Norman B.2,Dutter Michael3,Beachler David4,Kluber Todd5,Turner Robin6,Mateling Marian7,Lenters John8,Blanken Peter9,Maahn Maximilian10,Spence Christopher11,Kneifel Stefan12,Kucera Paul A.13,Tokay Ali14,Bliven Larry F.15,Wolff David B.15,Petersen Walter A.16

Affiliation:

1. NOAA/NESDIS/STAR/Advanced Satellite Products Branch, Madison, Wisconsin

2. Space Science and Engineering Center, University of Wisconsin–Madison, Madison, Wisconsin

3. NOAA/National Weather Service, Wakefield, Virginia

4. NOAA/National Weather Service, Indianapolis, Indiana

5. NOAA/National Weather Service, Chicago, Illinois

6. NOAA/National Weather Service, Marquette, Michigan

7. University of Wisconsin–Madison, Madison, Wisconsin

8. Michigan Technological University, Houghton, Michigan

9. Department of Geography, University of Colorado Boulder, Boulder, Colorado

10. Leipzig University, Leipzig, Germany

11. Environment and Climate Change Canada, Saskatoon, Saskatchewan, Canada

12. University of Cologne, Cologne, Germany

13. National Center for Atmospheric Research, Boulder, Colorado

14. NASA Goddard Space Flight Center, Greenbelt, Maryland

15. NASA Wallops Flight Facility, Wallops Island, Virginia

16. NASA Marshall Space Flight Center, Huntsville, Alabama

Abstract

AbstractA multisensor snowfall observational suite has been deployed at the Marquette, Michigan, National Weather Service Weather Forecast Office (KMQT) since 2014. Micro Rain Radar (MRR; profiling radar), Precipitation Imaging Package (PIP; snow particle imager), and ancillary ground-based meteorological observations illustrate the unique capabilities of these combined instruments to document radar and concomitant microphysical properties associated with northern Great Lakes snowfall regimes. Lake-effect, lake-orographic, and transition event case studies are presented that illustrate the variety of snowfall events that occur at KMQT. Case studies and multiyear analyses reveal the ubiquity of snowfall produced by shallow events. These shallow snowfall features and their distinctive microphysical fingerprints are often difficult to discern with conventional remote sensing instruments, thus highlighting the scientific and potential operational value of MRR and PIP observations. The importance of near-surface lake-orographic snowfall enhancement processes in extreme snowfall events and regime-dependent snow particle microphysical variability controlled by regime and environmental factors are also highlighted.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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