A spatial and temporal analysis of 30-day heavy snowfall amounts in the Eastern United States, 1900-2016

A spatial and temporal analysis of 30-day heavy snowfall amounts in the Eastern United States,... AbstractHeavy 30-day snowfall amounts were evaluated to identify spatial and temporal characteristics east of the Rockies in the United States during the period 1900-2016. An extensive data assessment identified 507 stations for use in this long-term climate study. The top 30-day heavy snowfall amount and the average of the top five 30-day heavy snowfall amounts were examined. Both amounts generally increased with latitude, however, much higher amounts were found downwind of the Great Lakes, at higher elevations, or in locations impacted by topographic features (e.g., Rockies, Black Hills, Appalachians). When compared to the 1981-2010 average winter snowfall, the top 30-day amount was found to be greater than the winter average in most areas of the Eastern U.S. The number of stations experiencing a top five 30-day heavy snowfall period in a winter ranged from one to 128 (1959/60), with a greater overall occurrence in the second half of the 117-year period. Six episodes had 10% or more stations experiencing one of the top five 30-day snowfall amounts, with the Feb-March 1960 episode impacting 124 stations, and these episodes were associated with large negative 500 hPA height anomalies. The northern Great Plains, Great Lakes, Midwest, and Northeast experienced more top five periods in the second half of the 117-year period, where most of the southern states experienced top five periods throughout the study period. Examining extremes at periods beyond the daily event and less than the season contributes to our knowledge of climate and provides useful information to snow-sensitive sectors. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Hydrometeorology American Meteorological Society

A spatial and temporal analysis of 30-day heavy snowfall amounts in the Eastern United States, 1900-2016

Journal of Hydrometeorology , Volume preprint (2017): 1 – Dec 4, 2017

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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1525-7541
D.O.I.
10.1175/JAMC-D-17-0217.1
Publisher site
See Article on Publisher Site

Abstract

AbstractHeavy 30-day snowfall amounts were evaluated to identify spatial and temporal characteristics east of the Rockies in the United States during the period 1900-2016. An extensive data assessment identified 507 stations for use in this long-term climate study. The top 30-day heavy snowfall amount and the average of the top five 30-day heavy snowfall amounts were examined. Both amounts generally increased with latitude, however, much higher amounts were found downwind of the Great Lakes, at higher elevations, or in locations impacted by topographic features (e.g., Rockies, Black Hills, Appalachians). When compared to the 1981-2010 average winter snowfall, the top 30-day amount was found to be greater than the winter average in most areas of the Eastern U.S. The number of stations experiencing a top five 30-day heavy snowfall period in a winter ranged from one to 128 (1959/60), with a greater overall occurrence in the second half of the 117-year period. Six episodes had 10% or more stations experiencing one of the top five 30-day snowfall amounts, with the Feb-March 1960 episode impacting 124 stations, and these episodes were associated with large negative 500 hPA height anomalies. The northern Great Plains, Great Lakes, Midwest, and Northeast experienced more top five periods in the second half of the 117-year period, where most of the southern states experienced top five periods throughout the study period. Examining extremes at periods beyond the daily event and less than the season contributes to our knowledge of climate and provides useful information to snow-sensitive sectors.

Journal

Journal of HydrometeorologyAmerican Meteorological Society

Published: Dec 4, 2017

References

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