The effect of the Arctic oscillation and North Atlantic oscillation on the frequency of significant snowfall events on the East Coast

Access to thesis restricted until 7/2023. Significant snowfall events are a serious disruptor along the east coast of the United States. Major snow events impact the health of citizens, transportation, and the economy. One of the problems that we face is that budgets for snowfall removal are driven...

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Bibliographic Details
Main Author: Goldstein, Jeremy P.
Other Authors: Call, David A.
Language:unknown
Published: 2020
Subjects:
Online Access:http://cardinalscholar.bsu.edu/handle/20.500.14291/202484
https://hdl.handle.net/20.500.14291/202484
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Summary:Access to thesis restricted until 7/2023. Significant snowfall events are a serious disruptor along the east coast of the United States. Major snow events impact the health of citizens, transportation, and the economy. One of the problems that we face is that budgets for snowfall removal are driven more by the number of events rather than total snowfall. A key issue forecasters face is predicting the number of significant snow events in a given winter season. Long-term forecasting, however, has improved significantly in the last few decades. Teleconnections or large scale variability patterns have been shown to give forecasters a good idea of how severe the winter season will be. For example, shifts in the jet stream are highly correlated with the phase of the teleconnection pattern. Although previous studies have shown connections between the phase of these teleconnections and the annual winter snowfall, little has been done to show if there is a connection between the phase of the teleconnections and the frequency of significant snowfall events. There has also been little research done on the annual variability in the number of significant snowfall events per season in recent years. A statistical analysis revealed that a weak negative relationship exists between the value of the teleconnection and the number of significant event days on the annual time scale and a moderate negative relationship exists on a monthly scale. An observational analysis of the annual variability showed that there is a notable amount of seasonal variability in the number of significant snowfall event days per season. A cluster analysis found that there was generally a higher number of significant snowfall event days in the north but in some years the southern states contributed more to the significant snowfall days than the northern states. Thesis (M.S.) Department of Geography