Weather Alert in Colorado
Avalanche Watch issued February 10 at 4:38PM MST by NWS Denver CO
AREAS AFFECTED: Elkhead and Park Mountains; West Elk and Sawatch Mountains; Flat Tops; West Jackson and West Grand Counties Above 9000 Feet
DESCRIPTION: AVABOU THE FOLLOWING MESSAGE IS TRANSMITTED AT THE REQUEST OF THE COLORADO AVALANCHE INFORMATION CENTER. AVALANCHE WATCH IN EFFECT FROM 5:00 PM TUESDAY UNTIL 5:00 PM WEDNESDAY *WHAT Dangerous avalanche conditions are taking shape. Expect the Avalanche Danger to rise to HIGH (Level 4 of 5) by late Wednesday evening. *WHERE Park Range, Flat Tops, Elk heads, and Ruby Raggeds *WHEN Expect dangerous avalanche conditions to begin overnight Wednesday and last through Thursday. *IMPACTS Heavy snow and wind, drifting snow, will create dangerous avalanche conditions. Large and dangerous avalanches will be easy to trigger once the new snow accumulates. Avalanches will run naturally. *PRECAUTION/PREPAREDNESS ACTIONS Travel in backcountry avalanche terrain is not recommended on THURSDAY. Avoid travel on and under slopes with a slope angle steeper than about 30 degrees. You can find more detailed information at colorado.gov/avalanche Davis
INSTRUCTION: N/A
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Weather Topic: What is Rain?
Home - Education - Precipitation - Rain
Next Topic: Shelf Clouds
Precipitation in the form of water droplets is called rain.
Rain generally has a tendency to fall with less intensity over a greater period
of time, and when rainfall is more severe it is usually less sustained.
Rain is the most common form of precipitation and happens with greater frequency
depending on the season and regional influences. Cities have been shown to have
an observable effect on rainfall, due to an effect called the urban heat island.
Compared to upwind, monthly rainfall between twenty and forty miles downwind of
cities is 30% greater.
Next Topic: Shelf Clouds
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
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