Weather Alert in New York
Flood Warning issued March 31 at 10:42PM EDT until April 1 at 7:00PM EDT by NWS Buffalo NY
AREAS AFFECTED: Monroe, NY
DESCRIPTION: * WHAT...Flooding caused by excessive rainfall continues along Irondequoit Creek. * WHERE...A portion of western New York, including the following county, Monroe. * WHEN...Until 700 PM EDT Wednesday. * IMPACTS...Flooding of low-lying and flood-prone locations along Irondequoit Creek is imminent or occurring. Widespread flooding will continue in Ellison Park, and flooding may also impact Panorama Plaza and portions of Blossom Road. * ADDITIONAL DETAILS... - At 1037 PM EDT, gauge reports indicated heavy rain due to thunderstorms with Irondequoit Creek approaching 9.5 feet. The creek will continue to rise overnight, and may approach the flood of record at 10 feet which occurred in July 1998. - Some locations that will experience flooding include... areas along Irondequoit Creek in Irondequoit, East Rochester, Fairport, Brighton and Penfield. - http://www.weather.gov/safety/flood
INSTRUCTION: Turn around, don't drown when encountering flooded roads. Most flood deaths occur in vehicles.
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 Altocumulus Clouds?
Home - Education - Cloud Types - 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
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
Current conditions powered by WeatherAPI.com
