Weather Alert in Nevada

Recent Locations: Holcomb, MS   Davis Junction, IL   Henderson, NV  

Hydrologic Outlook issued August 25 at 2:22AM PDT by NWS Elko NV

AREAS AFFECTED: Elko, NV; Eureka, NV

DESCRIPTION: ESFLKN Deep, monsoonal moisture will continue to stream northward into Northern and Central Nevada today through Thursday, resulting in the likelihood of wetting thunderstorms each afternoon and evening. Slow storm motions may produce heavy rainfall and localized flooding. Of particular concern are recent, large burn scars, including the Snowstorm Complex near Midas, the Cottonwood Peak fire north of Tuscarora, the Hot Canyon fire northwest of Montello, and the Adobe fire north of Elko. Numerous smaller burn scars from this fire season also remain vulnerable. Residents near recent burned scars should have multiple ways to receive Flash Flood Warnings and be prepared to act quickly. Travelers and recreationists should also remain alert and consider alternate plans.

INSTRUCTION: N/A

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Weather Topic: What is Sleet?

Home - Education - Precipitation - Sleet

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

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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