Weather Alert in Oklahoma
Severe Thunderstorm Warning issued March 4 at 7:28AM CST until March 4 at 8:15AM CST by NWS Tulsa OK
AREAS AFFECTED: McIntosh, OK; Muskogee, OK; Wagoner, OK
DESCRIPTION: SVRTSA The National Weather Service in Tulsa has issued a * Severe Thunderstorm Warning for... Northeastern McIntosh County in southeastern Oklahoma... Southeastern Wagoner County in northeastern Oklahoma... Northern Muskogee County in east central Oklahoma... * Until 815 AM CST. * At 728 AM CST, a severe thunderstorm was located 4 miles south of Council Hill, moving northeast at 45 mph. HAZARD...60 mph wind gusts and half dollar size hail. SOURCE...Radar indicated. IMPACT...Hail damage to vehicles is expected. Expect wind damage to roofs, siding, and trees. * Locations in or near the path include... Wainwright... Rentiesville... Hitchita... Greenleaf State Park... Oktaha... Summit... Pumpkin Center... Fort Gibson... Muskogee... Braggs... Okay... Pierce... Council Hill... Checotah... Lake Eufaula State Park... Keefeton... This includes Interstate 40 in Oklahoma between mile markers 251 and 267.
INSTRUCTION: For your protection move to an interior room on the lowest floor of a building.
Want more detail? Get the Complete 7 Day and Night Detailed Forecast!
Current U.S. National Radar--Current
The Current National Weather Radar is shown below with a UTC Time (subtract 5 hours from UTC to get Eastern Time).
National Weather Forecast--Current
The Current National Weather Forecast and National Weather Map are shown below.
National Weather Forecast for Tomorrow
Tomorrow National Weather Forecast and Tomorrow National Weather Map are show below.
North America Water Vapor (Moisture)
This map shows recent moisture content over North America. Bright and colored areas show high moisture (ie, clouds); brown indicates very little moisture present; black indicates no moisture.
Weather Topic: What are Stratocumulus Clouds?
Home - Education - Cloud Types - 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
Weather Topic: What are Wall Clouds?
Home - Education - Cloud Types - Wall Clouds
Next Topic: Altocumulus Clouds
A wall cloud forms underneath the base of a cumulonimbus cloud,
and can be a hotbed for deadly tornadoes.
Wall clouds are formed by air flowing into the cumulonimbus clouds, which can
result in the wall cloud descending from the base of the cumulonimbus cloud, or
rising fractus clouds which join to the base of the storm cloud as the wall cloud
takes shape.
Wall clouds can be very large, and in the Northern Hemisphere they generally
form at the southern edge of cumulonimbus clouds.
Next Topic: Altocumulus Clouds
Current conditions powered by WeatherAPI.com
