Weather Alert in Nevada

Recent Locations: West Topsham, VT   Bruno, MN   Blue Diamond, NV  

Hydrologic Outlook issued August 22 at 11:29PM PDT by NWS Elko NV

AREAS AFFECTED: Elko, NV; Eureka, NV

DESCRIPTION: ESFLKN Deep, monsoonal moisture will surge northward into most of Northern and Central Nevada Sunday afternoon through Wednesday evening. As a result, showers and thunderstorms will develop across much of Northern and Central Nevada each afternoon and evening Sunday through Wednesday. Slow storm motions may result in heavy rainfall and localized flooding. Of great concern will be recent, large burn scars left from the following incidents: 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 other smaller burn scars have been created this past fire season and are also of concern. If living near recently burned areas, please have a way to receive flash flood warnings and be prepared to take action should warnings be issued. If you are traveling or recreating in areas that have burn scars, please consider changing plans.

INSTRUCTION: N/A

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Weather Topic: What are Altocumulus Clouds?

Home - Education - Cloud Types - Altocumulus Clouds

Altocumulus Clouds Next Topic: Altostratus Clouds

Similar to cirrocumulus clouds, altocumulus clouds are characterized by cloud patches. They are distinguished by larger cloudlets than cirrocumulus clouds but are still smaller than stratocumulus clouds.

Altocumulus clouds most commonly form in middle altitudes (between 2 and 5 km) and may resemble, at times, the shape of a flying saucer. These uncommon formations, called altocumulus lenticularis, are created by uplift in the atmosphere and are most often seen in close proximity to mountains.

Next Topic: Altostratus Clouds

Weather Topic: What are Cirrocumulus Clouds?

Home - Education - Cloud Types - Cirrocumulus Clouds

Cirrocumulus Clouds Next Topic: Cirrostratus Clouds

Cirrocumulus clouds form at high altitudes (usually around 5 km) and have distinguishing characteristics displayed in a fine layer of small cloud patches. These small cloud patches are sometimes referred to as "cloudlets" in relation to the whole cloud formation.

Cirrocumulus clouds are formed from ice crystals and water droplets. Often, the water droplets in the cloud freeze into ice crystals and the cloud becomes a cirrostratus cloud. Because of this common occurrence, cirrocumulus cloud formations generally pass rapidly.

Next Topic: Cirrostratus Clouds

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