19 Progress Toward Understanding Present and Past River Responses to Climate in Eastern and Midwestern North America
Sunday, 19 March 2017
1:30 PM - 3:30 PM
Allegheny, 17th Floor
DEVELOPMENT OF A FLOOD CLIMATOLOGY FOR THE UPPER ALLEGHENY RIVER BASIN IN NORTHWESTERN PENNSYLVANIA
Paper number: 19-6
Program: Theme Sessions
Time: 3:10 PM – 3:30 PM
Authors
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Todd GroteIndiana University Southeast, New Albany, IN
Abstract
Composites of uARB USGS-HCDN station records show that 59% of flood events occur from December to March, with March flooding contributing the highest portion of the total (~22%). Conversely, flooding is least common during August, which experiences only 2% of peak annual flows. Annual peak flows from 1995-96 through 2014-15 are dominated by snowmelt or rain-on-snow events (~65%), primarily from December through March. Flooding from synoptic scale frontal passages, including convective precipitation and orographically enhanced events that produce extreme rainfall rates in some cases, are responsible for generating (~26%) of flooding throughout the uARB. Although rare (~ 4%), tropical systems have produced very large annual maximum floods. Understanding seasonal variations in flooding and the development of a flood climatology for the uARB are important pieces of information for flood forecasting, flood hazard assessment, and water resource management.
Geological Society of America Abstracts with Programs. Vol. 49, No. 2
doi: 10.1130/abs/2017NE-291450
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