Weather Alert in Indiana
Beach Hazards Statement issued August 21 at 4:40AM EDT until August 21 at 2:00PM EDT by NWS Northern Indiana
AREAS AFFECTED: Northern La Porte
DESCRIPTION: * WHAT...Dangerous swimming conditions expected. * Waves: Waves 3 to 5 feet this morning will subside to 1 to 2 feet by mid afternoon. * Life-threatening rip and structural currents expected, especially on the north sides of piers and breakwalls. * A strong longshore current flowing from north to south is expected. * WHERE...In Indiana, Northern La Porte county. In Michigan, Southern Berrien county. * WHEN...Until 1 PM CDT this afternoon. * IMPACTS...Strong currents can pull swimmers into deeper water and high waves can sweep people off piers.
INSTRUCTION: Remain out of the water to avoid hazardous swimming conditions. Do not venture out on piers.
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Weather Topic: What is Snow?
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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.
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