Weather Alert in Montana
Hydrologic Outlook issued March 24 at 11:31AM MDT by NWS Missoula MT
AREAS AFFECTED: Lincoln, MT; Mineral, MT; Sanders, MT
DESCRIPTION: ESFMSO Lincoln, Sanders and Mineral Counties Moderate rainfall is expected to continue across the region through Wednesday morning. With the ground already saturated and local creeks and streams running high and fast from recent rains, this additional precipitation may lead to minor hydrologic issues such as: Minor over bank flows along smaller, quick-responding creeks and streams; localized ponding of water in low-lying and poor drainage areas; and standing water on some roadways, particularly in familiar trouble spots. Widespread flooding is not anticipated at this time. However, those living near waterways or in areas prone to nuisance flooding should monitor the situation.
INSTRUCTION: N/A
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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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