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dc.date.accessioned2022-05-09T00:50:19Z
dc.date.available2022-05-09T00:50:19Z
dc.date.copyright21 Jan 2022
dc.date.issued2022
dc.identifier.otherWAF-D-21-0085.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4285619
dc.description.abstractFreezing rain can cause significant tree damage with fallen trees and branches blocking roads and taking power distribution lines out of service. Power transmission lines are designed for ice loads from freezing rain, using models to estimate equivalent radial ice thicknesses from historical weather data. The conservative simple flux model assumes that all the freezing rain that impinges on a horizontal cylinder, representing vegetation or components of the built infrastructure, freezes. Here I present a simplified heat-balance formulation to calculate the fraction of the impinging precipitation that freezes, using parameters measured at ASOS weather stations and an estimate of solar heating. Radial ice thickness estimates from this approach are compared with the simple model and those generated from the ASOS icing sensor. These estimates can all be tested by comparing to measurements on cylinders at weather stations. A link to an Excel spreadsheet that calculates freezing fraction using user-input weather data is provided. In forecast freezing rain events, this tool could be used by utility crews and emergency response teams to estimate the likely range of equivalent radial ice thicknesses over the affected region and plan their response accordingly.
dc.titleFreezing Fraction in Freezing Rain
dc.typeJournal Paper
dc.journal.volume37
dc.journal.issue1
dc.journal.titleWeather and Forecasting
dc.identifier.doi10.1175/WAF-D-21-0085.1
dc.page163–178
dc.treeWeather and Forecasting:;2022:;volume( 037 ):;issue: 001
dc.contenttypeFulltext


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