Weather Alert in Colorado
Avalanche Watch issued March 31 at 9:43AM MDT by NWS Denver CO
AREAS AFFECTED: Gore and Elk Mountains/Central Mountain Valleys; West Elk and Sawatch Mountains
DESCRIPTION: AVABOU THE FOLLOWING MESSAGE IS TRANSMITTED AT THE REQUEST OF THE COLORADO AVALANCHE INFORMATION CENTER. AVALANCHE WATCH IN EFFECT FROM 8 AM TUESDAY UNTIL 5 PM TUESDAY *WHAT Dangerous avalanche conditions develop on Tuesday morning and last through the day. Expect the Avalanche Danger to rise to HIGH (Level 4 of 5). *WHERE Elk Mountains. *WHEN Expect very dangerous avalanche conditions to begin on Tuesday morning by about 8:00 AM and last until 5:00 PM. *IMPACTS High snowfall rates and strong winds will create dangerous avalanche conditions by Tuesday morning. Large and dangerous avalanches will be easy to trigger once the new snow accumulates. Avalanches will run naturally. Pritchett
INSTRUCTION: N/A
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Weather Topic: What is Sleet?
Home - Education - Precipitation - Sleet
Next Topic: Snow
Sleet is a form of precipitation in which small ice pellets are the primary
components. These ice pellets are smaller and more translucent than hailstones,
and harder than graupel. Sleet is caused by specific atmospheric conditions and
therefore typically doesn't last for extended periods of time.
The condition which leads to sleet formation requires a warmer body of air to be
wedged in between two sub-freezing bodies of air. When snow falls through a warmer
layer of air it melts, and as it falls through the next sub-freezing body of air
it freezes again, forming ice pellets known as sleet. In some cases, water
droplets don't have time to freeze before reaching the surface and the result is
freezing rain.
Next Topic: Snow
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
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