Weather Alerts for Idaho
1. Extreme Heat Warning for: Lewiston Area; Lower Garfield and Asotin Counties
2. Heat Advisory for: Lewis and Southern Nez Perce Counties
3. Heat Advisory for: Lower Treasure Valley; Malheur County; Oregon Lower Treasure Valley
4. Heat Advisory for: Northern Panhandle; Coeur d'Alene Area; Idaho Palouse; Central Panhandle Mountains; Washington Palouse; Spokane Area; Northeast Mountains
5. Heat Advisory for: Orofino/Grangeville Region; Lower Hells Canyon/Salmon River Region
6. Heat Advisory for: Upper Treasure Valley
7. Red Flag Warning for: East Salmon River Mountains/Salmon NF; Lemhi and Lost River Range/Challis NF
8. Red Flag Warning for: Palouse/Nezperce Reservation/Hells Canyon Region
9. Red Flag Warning for: Sawtooth Range/Northern Sawtooth NF; Middle Snake River Valley/Twin Falls BLM north of the Snake River; Goose Creek and Raft River Valley/Southern Sawtooth NF/Twin Falls BLM south of the Snake River
10. Red Flag Warning for: Upper Snake River Valley/Idaho Falls BLM; Centennial Mountains and Snake River Range/Targhee NF; Caribou Range/Caribou NF
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National Weather Forecast for Tomorrow
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North America Water Vapor (Moisture)
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Weather Topic: What is Evaporation?
Home - Education - Precipitation - Evaporation
Next Topic: Fog
Evaporation is the process which returns water from the earth
back to the atmosphere, and is another crucial process in the water cycle.
Evaporation is the transformation of liquid into gas, and it happens because
molecules are excited by the application of energy and turn into vapor.
In order for water to evaporate it has to be on the surface of a body of water.
Next Topic: Fog
Weather Topic: What are Fractus Clouds?
Home - Education - Cloud Types - Fractus Clouds
Next Topic: Freezing Rain
A fractus cloud (scud) is a fragmented, tattered cloud which has
likely been sheared off of another cloud. They are accessory clouds, meaning they
develop from parent clouds, and are named in a way which describes the original
cloud which contained them.
Fractus clouds which have originated from cumulus clouds are referred to as
cumulus fractus, while fractus clouds which have originated from stratus clouds
are referred to as stratus fractus. Under certain conditions a fractus cloud might
merge with another cloud, or develop into a cumulus cloud, but usually a
fractus cloud seen by itself will dissipate rapidly.
They are often observed on the leading and trailing edges of storm clouds,
and are a display of wind activity.
Next Topic: Freezing Rain
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