Weather Alert in Idaho
Air Quality Alert issued August 22 at 2:20PM PDT by NWS Spokane WA
AREAS AFFECTED: Latah, ID; Lewis, ID; Nez Perce, ID
DESCRIPTION: An Air Quality Alert has been issued by the following agencies: Idaho Department of Environmental Quality in Lewiston Nez Perce Tribe ERWM Air Quality Program * WHAT...Air Quality Advisory due to smoke from wildfires. Air Quality Index is forecast to be Unhealthy. * WHERE...Latah and Nez Perce Counties, and the Nez Perce Reservation. * WHEN...Until Monday morning August 25th. * IMPACTS...Those who experience health effects from smoke include children under 18, elders, pregnant women, people with asthma or have difficulty breathing, diabetes, heart problems or otherwise compromised health, and people who have high exposure (those who work, exercise, or spend extensive time outdoors).
INSTRUCTION: Under the most severe pollution level, sensitive groups should avoid outdoor exposure and limit indoor activities, and everyone should restrict their outdoor activities. Idaho Department of Health and Welfare https://healthandwelfare.idaho.gov/health-wellness/environmental- health/idaho-wildfire-and-smoke-information Idaho Smoke Information Hotline: 1-800-345-1007 Idaho DEQ Lewiston Regional Office - (208)-799-4370
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Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Weather Topic: What are Altostratus Clouds?
Home - Education - Cloud Types - Altostratus Clouds
Next Topic: Cirrocumulus Clouds
Altostratus clouds form at mid to high-level altitudes
(between 2 and 7 km) and are created by a warm, stable air mass which causes
water vapor
to condense as it rise through the atmosphere. Usually altostratus clouds are
featureless sheets characterized by a uniform color.
In some cases, wind punching through the cloud formation may give it a waved
appearance, called altostratus undulatus. Altostratus clouds
are commonly seen with other cloud formations accompanying them.
Next Topic: Cirrocumulus Clouds
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