Weather Alert in Nebraska
Special Weather Statement issued February 11 at 4:02AM CST by NWS Hastings NE
AREAS AFFECTED: Nance; Howard; Merrick; Polk; Hall; Hamilton
DESCRIPTION: Although not considered a significant concern, the threat for localized ice jam flooding cannot be ruled out for those portions of mainly the Loup, North Loup and Platte Rivers (downstream of Grand Island) where at least some ice is still present and gradually breaking up/moving downstream. Should any ice jams happen to develop, water levels could fluctuate as much as 1 to 3 feet in a short time, causing flooding with little, if any notice. This is especially true for known, ice jam prone locations. If any ice jam flooding is observed along the Loup, North Loup or Platte Rivers, please report it immediately to the National Weather Service in Hastings.
INSTRUCTION: N/A
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Weather Topic: What is Snow?
Home - Education - Precipitation - Snow
Next Topic: Stratocumulus Clouds
Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake,
has unique characteristics, but all of them grow in a hexagonal structure.
Snowfall can last for sustained periods of time and result in significant buildup
of snow on the ground.
On the earth's surface, snow starts out light and powdery, but as it begins to melt
it tends to become more granular, producing small bits of ice which have the consistency of
sand. After several cycles of melting and freezing, snow can become very dense
and ice-like, commonly known as snow pack.
Next Topic: Stratocumulus Clouds
Weather Topic: What are Stratus Clouds?
Home - Education - Cloud Types - Stratus Clouds
Next Topic: Wall Clouds
Stratus clouds are similar to altostratus clouds, but form at a
lower altitude and are identified by their fog-like appearance, lacking the
distinguishing features of most clouds.
Stratus clouds are wider than most clouds, and their base has a smooth, uniform
look which is lighter in color than a nimbostratus cloud.
The presence of a stratus cloud indicates the possibility of minor precipitation,
such as drizzle, but heavier precipitation does not typically arrive in the form
of a stratus cloud.
Next Topic: Wall Clouds
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