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Overview

Lead up: In the days leading up to this event, it became apparent that an unusual event was looming on the horizon as forecast models were increasingly hinting that a very strong Canadian cold front would develop over western Canada and plunge south across eastern Idaho. In fact, this is what indeed occurred. A cold front developed off of a westward extending tail that emanated from a Polar Vortex located south of Hudson Bay, Canada. Unusually cold air built up behind the front, and a tremendous amount of wind was developing in association with this system. The National Weather Service in Pocatello began to ramp up messaging in advance of this system once forecaster confidence became high. Two days before the event, forecasters created and sent targeted emails, social media posts and additional detailed posts in an Emergency Management portal. In addition, we partnered with the Idaho Transportation Department and Idaho State Communications to activate overhead message signs of the incoming winds, in an effort to encourage Labor Day travelers to reach their destinations early, prior to the onset of strong winds.

 

The event: During the early afternoon hours of Monday, September 7, the cold front entered Idaho from the north. The front then rapidly raced south, reaching the Arco Desert and Idaho Falls by 4PM, Pocatello by 5PM, then the eastern Magic Valley and Utah border by 7PM. Strong, damaging winds developed behind the front, pouring first through gaps in the Continental Divide then surging south behind the front. Widespread wind gusts out of the north/northeast in the 50-75 mph range were recorded along and behind the front, across all but Teton, Caribou and Bear Lake counties. Winds then continued through the night, with a secondary surge just after midnight. Although still remaining breezy, the damaging winds ceased around sunrise. Widespread tree and power line damage was reported, with thousands still without power 24 hours later. Structural damage occurred to outbuildings and some homes. In addition, several schools cancelled classes due to the power outages. This event contained many highly unusual factors, including the shear strength of the winds, the direction of the winds, the large area across which they occurred as well as how long they lasted. All these things combined suggest that there may not be another event comparable to this in eastern Idaho's climate history. We hope those that lost power and sustained damage can return to normal quickly.

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