Weather Alert in Kansas
Severe Thunderstorm Warning issued June 16 at 11:14PM CDT until June 16 at 11:45PM CDT by NWS Hastings NE
AREAS AFFECTED: Jewell, KS; Smith, KS; Franklin, NE; Webster, NE
DESCRIPTION: SVRGID The National Weather Service in Hastings has issued a * Severe Thunderstorm Warning for... Northwestern Jewell County in north central Kansas... Northeastern Smith County in north central Kansas... Western Webster County in south central Nebraska... Eastern Franklin County in south central Nebraska... * Until 1145 PM CDT. * At 1114 PM CDT, severe thunderstorms were located along a line extending from near Hildreth to near Franklin to 9 miles south of Bloomington, moving southeast at 45 mph. HAZARD...60 mph wind gusts and quarter size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Severe thunderstorms will be near... Riverton around 1120 PM CDT. Inavale around 1130 PM CDT. Other locations in the path of these severe thunderstorms include Smith Center.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
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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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