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contributor authorWhite, Allen B.
contributor authorMoore, Benjamin J.
contributor authorGottas, Daniel J.
contributor authorNeiman, Paul J.
date accessioned2019-09-22T09:03:43Z
date available2019-09-22T09:03:43Z
date copyright10/2/2018 12:00:00 AM
date issued2018
identifier otherBAMS-D-18-0091.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4262633
description abstractDuring winter 2016/17, California experienced numerous heavy precipitation events linked to land-falling atmospheric rivers (ARs) that filled reservoirs and ended a severe, multiyear drought. These events also caused floods, mudslides, and debris flows, resulting in major socioeconomic disruptions. During 2?11 February 2017, persistent heavy precipitation in the northern Sierra Nevada culminated in a rapid increase in the water level on Lake Oroville, necessitating the activation of an emergency spillway for the first time since the Oroville Dam was installed and forcing the evacuation of 188,000 people. The precipitation, which mostly fell as rain due to elevated freezing levels, was focused on the western slope of the Sierra Nevada in connection with orographic forcing linked to two successive ARs. Heavy rain fell on saturated soils and a snowpack produced by antecedent storms and thereby resulted in excessive runoff into Lake Oroville that led to a damaged spillway and complicated reservoir operations.
publisherAmerican Meteorological Society
titleWinter Storm Conditions Leading to Excessive Runoff above California’s Oroville Dam during January and February 2017
typeJournal Paper
journal volume100
journal issue1
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-D-18-0091.1
journal fristpage55
journal lastpage70
treeBulletin of the American Meteorological Society:;2018:;volume 100:;issue 001
contenttypeFulltext


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