Weather Alert in Connecticut

Recent Locations: Sunbury, OH   Ocotillo, CA   Tolland, CT  
Current Alerts for Tolland, CT: Special Weather Statement

Special Weather Statement issued March 6 at 9:32PM EST by NWS Boston/Norton MA

AREAS AFFECTED: Hartford; Tolland; Windham; Western Franklin; Eastern Franklin; Northern Worcester; Central Middlesex County; Western Essex; Eastern Essex; Western Hampshire; Western Hampden; Eastern Hampshire; Eastern Hampden; Southern Worcester; Western Norfolk; Southeast Middlesex; Suffolk; Eastern Norfolk; Northern Bristol; Western Plymouth; Eastern Plymouth; Southern Bristol; Southern Plymouth; Barnstable; Dukes; Northwest Middlesex County; Northwest Providence; Southeast Providence; Western Kent; Eastern Kent; Bristol; Washington; Newport

DESCRIPTION: Areas of drizzle with pockets of freezing drizzle will continue into early Saturday morning. The bulk of the freezing drizzle will be in the high terrain where temperatures were at or below freezing and untreated roads maybe icy. However...even some of the lower elevations had temperatures around 32 degrees which may lead to some patchy black ice. Plan on allowing extra travel time and be especially careful on bridges and overpasses. This is particularly true in the high terrain where temperatures were a few degrees below freezing. Pedestrians should also be careful in parking lots and walkways which may have patches of black ice. Temperatures will warm above freezing by mid to late Saturday morning alleviating any issues.

INSTRUCTION: N/A

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Weather Topic: What are Shelf Clouds?

Home - Education - Cloud Types - Shelf Clouds

Shelf Clouds Next Topic: Sleet

A shelf cloud is similar to a wall cloud, but forms at the front of a storm cloud, instead of at the rear, where wall clouds form.

A shelf cloud is caused by a series of events set into motion by the advancing storm; first, cool air settles along the ground where precipitation has just fallen. As the cool air is brought in, the warmer air is displaced, and rises above it, because it is less dense. When the warmer air reaches the bottom of the storm cloud, it begins to cool again, and the resulting condensation is a visible shelf cloud.

Next Topic: Sleet

Weather Topic: What is Snow?

Home - Education - Precipitation - Snow

Snow Next Topic: Stratocumulus Clouds

Snow is precipitation taking the form of ice crystals. Each ice crystal, or snowflake, has unique characteristics, but all of them grow in a hexagonal structure. Snowfall can last for sustained periods of time and result in significant buildup of snow on the ground.

On the earth's surface, snow starts out light and powdery, but as it begins to melt it tends to become more granular, producing small bits of ice which have the consistency of sand. After several cycles of melting and freezing, snow can become very dense and ice-like, commonly known as snow pack.

Next Topic: Stratocumulus Clouds

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