Weather Alert in North Carolina

Recent Locations: Perryopolis, PA   Raleigh, NC  
Current Alerts for Raleigh, NC: Special Weather Statement

Special Weather Statement issued March 28 at 7:25PM EDT by NWS Newport/Morehead City NC

AREAS AFFECTED: Martin; Pitt; Washington; Greene; Beaufort; Duplin; Lenoir; Jones; Northern Craven

DESCRIPTION: The combination of afternoon relative humidity values 30 to 35% and very dry fine fuels will result in an increased risk for the spread of wildfires Sunday afternoon across interior Eastern North Carolina. Everyone is urged to properly dispose of cigarette butts, matches, and any other flammable items in appropriate containers. Additionally, exercise caution if operating any equipment that could create sparks, and keep vehicles off of dry grass. Most dry grasses, dead leaves, and other tree litter could easily ignite and spread fire quickly. A statewide burn ban issued by the North Carolina Forest Service is currently in place. All open burning is prohibited until further notice.

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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