Weather Alerts for Oregon
1. Dense Fog Advisory for: Clatsop County Coast; Tillamook County Coast; Central Coast of Oregon; South Washington Coast
2. Extreme Heat Warning for: Eastern Curry County and Josephine County; Jackson County
3. Heat Advisory for: Central Douglas County
4. Heat Advisory for: Oregon Lower Treasure Valley
5. Red Flag Warning for: Canyon Grassland of Wallowa County; Kittitas Valley; Lower Columbia Basin; Blue Mountains of Washington; Southeast Washington Grande Ronde Valley; Yakama Alpine District
6. Red Flag Warning for: John Day Valley; Southern Blue Mountains; Central Mountains of Oregon; Warm Springs Reservation; Northern Deschutes National Forest; Southern Deschutes National Forest
7. Red Flag Warning for: Klamath Basin and the Fremont-Winema National Forest
8. Red Flag Warning for: Lower Columbia Basin of Oregon; Eastern Columbia River Gorge of Oregon; East Slopes of Mount Hood National Forest
9. Red Flag Warning for: Western Rogue Basin including the Illinois Valley; Eastern Rogue Valley
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Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - Stratocumulus Clouds
Next Topic: Stratus Clouds
Stratocumulus clouds are similar to altocumulus clouds in their
fluffy appearance, but have a slightly darker shade due to their additional mass.
A good way to distinguish the two cloud types is to hold your hand out and measure
the size of an individual cloud; if it is the size of your thumb it is generally
an altocumulus cloud, if it is the size of your hand it is generally a
stratocumulus cloud.
It is uncommon for stratocumulus clouds to produce precipitation, but if they do
it is usually a light rain or snow.
Next Topic: Stratus Clouds
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
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