Weather Alert in Nebraska
Flood Advisory issued February 10 at 2:13AM CST until February 10 at 12:00PM CST by NWS Hastings NE
AREAS AFFECTED: Hall, NE; Hamilton, NE; Merrick, NE
DESCRIPTION: * WHAT...Flooding caused by an ice jam continues. * WHERE...Portions of central and south central Nebraska, including the following counties, in central Nebraska, Merrick. In south central Nebraska, Hall and Hamilton. * WHEN...Until noon CST Tuesday. * IMPACTS...Minor flooding in low-lying areas and pastures/fields along the Platte River. * ADDITIONAL DETAILS... - At 158 AM CST, within the last 24 hours, National Weather Service personnel and the public reported an ice jam within one of the channels of the Platte River southeast of Grand Island, with the jam centered in an area between South Locust Street and Highway 34. Minor flooding has already occurred, and will likely continue in this area through at least sometime Tuesday. - Please note that the duration and extent of ice jam flooding is difficult to predict, as ice jams can develop and break free with little notice, causing water levels to fluctuate up to a few feet in a short time. - Some locations that could experience flooding include... Low lying areas and pasture/farm ground adjacent to the Platte River in rural Hall, Hamilton, and Merrick Counties. - http://www.weather.gov/safety/flood
INSTRUCTION: Be aware of your surroundings and do not drive on flooded roads.
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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
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