Overview of Ice Jams in Three Major US Rivers

We investigated ice jams on the Yukon, the Platte, and the Connecticut Rivers. Information on the dates of jam occurrence and the latitude and longitude of each jam was found in the Ice Jam Database (www.crrel.usace.army.mil/icejams/). Information was available for 255 ice jams on the Platte River,...

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Bibliographic Details
Main Authors: Steven F. Daly, Carrie Vuyovich
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2007
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.599.2924
http://cripe.civil.ualberta.ca/Downloads/14th_Workshop/Daly-Vuyovich-2007.pdf
Description
Summary:We investigated ice jams on the Yukon, the Platte, and the Connecticut Rivers. Information on the dates of jam occurrence and the latitude and longitude of each jam was found in the Ice Jam Database (www.crrel.usace.army.mil/icejams/). Information was available for 255 ice jams on the Platte River, 210 ice jams on the Yukon River; and 94 ice jams on the Connecticut River. Each ice jam was associated with the closest NWS meteorological station and the closest downstream USGS gaging station for which there were consistent records. The daily discharge and the accumulated freezing degree days (AFDD) associated with each ice jam event along with the changes in discharge and AFDD in the time period immediately prior to each event were determined. As the majority of entries in the database have been entered with "Unknown " type, the type of jam was determined independently for each ice event based on the flow conditions immediately prior to the jam formation and the time of year that the jam occurred. Ice jams were classified as freezeup jams if the river discharge decreased prior to the ice jam formation, as indicated by the change in discharge over the previous 5 days. Any jam not classified as a freezeup jam was classified as a breakup jam. Surveys of the day-of-year and discharge for each ice jam location along the entire length of each river are presented. Information on the day-of-year was used to classify the jam formation as progressive (Yukon), semi-progressive (Platte) or non-progressive (Connecticut). Histograms of freezeup and breakup jams by the day-of-year and discharge show that the classification of jam type by discharge produces consistent and rational results