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WHAT: Flash flooding and debris flows caused by excessive rainfall continue to be possible over the Wapiti Burn Area.
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WHERE: A portion of southwest Idaho, including the following area, Boise Mountains.
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WHEN: Until 9 PM MDT this evening.
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IMPACTS: Heavy rainfall over the Wapiti Burn Area is expected up to and during the period of the watch. Residents near the Wapiti Burn Area should prepare for potential flooding impacts. Be sure to stay up to date with information from local authorities. Heavy rainfall could trigger flash flooding or debris flows in and near recent wildfire burn scars.
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ADDITIONAL DETAILS:
- National Weather Service Meteorologists are forecasting heavy rainfall over the Wapiti Burn Area, which may lead to flash flooding and debris flows.
- https://www.weather.gov/safety/flood
* WHAT...Flash flooding and debris flows caused by excessive rainfall continue to be possible over the Wapiti Burn Area. * WHERE...A portion of southwest Idaho, including the following area, Boise Mountains. * WHEN...Until 9 PM MDT this evening. * IMPACTS...Heavy rainfall over the Wapiti Burn Area is expected up to and during the period of the watch. Residents near the Wapiti Burn Area should prepare for potential flooding impacts. Be sure to stay up to date with information from local authorities. Heavy rainfall could trigger flash flooding or debris flows in and near recent wildfire burn scars. * ADDITIONAL DETAILS... - National Weather Service Meteorologists are forecasting heavy rainfall over the Wapiti Burn Area, which may lead to flash flooding and debris flows. - https://www.weather.gov/safety/flood
You should monitor later forecasts and be prepared to take action should Flash Flood Warnings be issued.
Avertizările de vreme severă sunt furnizate către meteoblue de peste 80 de agenții oficiale din întreaga lume. meteoblue nu își asumă nicio responsabilitate privind conținutul sau natura avertizărilor. Problemele pot fi raportate prin intermediul formularului nostru de feedback și vor fi transmise instituțiilor competente.
