The Role of Sublimational Cooling in a Late-Season Midwestern Snow Event
| dc.contributor.author | Market, Patrick S. | |
| dc.contributor.author | Przybylinksi, Ronald W. | |
| dc.contributor.author | Rochette, Scott M. | |
| dc.date.accessioned | 2021-09-07T17:37:59Z | |
| dc.date.available | 2021-09-07T17:37:59Z | |
| dc.date.issued | 2006-06-01 | |
| dc.identifier.citation | Market, P. S., Przybylinski, R. W., and Rochette, S. M., 2006, The Role of Sublimational Cooling in a Late-season Midwestern Snow Event, Wea. Forecasting , 21, 364-382. Available on publisher's site at http://journals.ametsoc.org/doi/abs/10.1175/WAF919.1 . | |
| dc.identifier.doi | https://doi.org/10.1175/WAF919.1 | |
| dc.identifier.uri | http://hdl.handle.net/20.500.12648/2195 | |
| dc.description | Copyright 2006 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act September 2010 Page 2 or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (http://www.ametsoc.org/) or from the AMS at 617-227-2425 or copyright@ametsoc.org. | |
| dc.description.abstract | Analysis is provided of a surprise late-season snow event over eastern Missouri and western Illinois. While snow totals failed to exceed 15 cm (6 in.) at any single location, the system was noteworthy because of the poor performance of public, private, and media forecasts in anticipating the event. Using observed data and a successful simulation with a mesoscale numerical model, the event is scrutinized to determine the forcing mechanisms for the precipitation over a small area. A region of enhanced frontogenesis is diagnosed over the region both in the observed data as well as the model output. That the precipitation fell as snow is shown to be the result of a dry layer of air between the surface and the cloud base that saturated and cooled due largely to snow sublimation–evaporation in just a few hours to permit the fall of snow uninhibited from the cloud base to the ground. | |
| dc.title | The Role of Sublimational Cooling in a Late-Season Midwestern Snow Event | |
| dc.type | article | |
| dc.source.journaltitle | Weather and Forecasting | |
| dc.source.volume | 21 | |
| dc.source.issue | 3 | |
| refterms.dateFOA | 2021-09-07T17:37:59Z | |
| dc.description.institution | SUNY Brockport | |
| dc.source.peerreviewed | TRUE | |
| dc.source.status | published | |
| dc.description.publicationtitle | Earth Sciences Faculty Publications | |
| dc.contributor.organization | National Weather Service | |
| dc.contributor.organization | The College at Brockport | |
| dc.contributor.organization | University of Missouri - Columbia | |
| dc.languate.iso | en_US |
