Weather Alert in Kansas
Severe Thunderstorm Watch issued June 16 at 11:16PM CDT until June 17 at 7:00AM CDT by NWS Topeka KS
AREAS AFFECTED: Brown, KS; Clay, KS; Cloud, KS; Dickinson, KS; Geary, KS; Jackson, KS; Lyon, KS; Marshall, KS; Morris, KS; Nemaha, KS; Osage, KS; Ottawa, KS; Pottawatomie, KS; Republic, KS; Riley, KS; Shawnee, KS; Wabaunsee, KS; Washington, KS
DESCRIPTION: THE NATIONAL WEATHER SERVICE HAS ISSUED SEVERE THUNDERSTORM WATCH 425 IN EFFECT UNTIL 7 AM CDT TUESDAY FOR THE FOLLOWING AREAS IN KANSAS THIS WATCH INCLUDES 18 COUNTIES IN CENTRAL KANSAS DICKINSON IN EAST CENTRAL KANSAS GEARY LYON MORRIS OSAGE SHAWNEE WABAUNSEE IN NORTH CENTRAL KANSAS CLAY CLOUD OTTAWA REPUBLIC WASHINGTON IN NORTHEAST KANSAS BROWN JACKSON MARSHALL NEMAHA POTTAWATOMIE RILEY THIS INCLUDES THE CITIES OF ABILENE, ALMA, ALTA VISTA, BELLEVILLE, BENNINGTON, BLUE RAPIDS, BURLINGAME, CARBONDALE, CLAY CENTER, CLIFTON, CONCORDIA, COUNCIL GROVE, EMPORIA, ESKRIDGE, FRANKFORT, GREENLEAF, HANOVER, HARVEYVILLE, HERINGTON, HIAWATHA, HOLTON, HORTON, JUNCTION CITY, LINN, LYNDON, MANHATTAN, MAPLE HILL, MARYSVILLE, MCFARLAND, MINNEAPOLIS, OSAGE CITY, OVERBROOK, PAXICO, SABETHA, SENECA, ST. MARYS, TOPEKA, WAMEGO, AND WASHINGTON.
INSTRUCTION: N/A
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Weather Topic: What is Precipitation?
Home - Education - Precipitation - Precipitation
Next Topic: Rain
Precipitation can refer to many different forms of water that
may fall from clouds. Precipitation occurs after a cloud has become saturated to
the point where its water particles are more dense than the air below the cloud.
In most cases, precipitation will reach the ground, but it is not uncommon for
precipitation to evaporate before it reaches the earth's surface.
When precipitation evaporates before it contacts the ground it is called Virga.
Graupel, hail, sleet, rain, drizzle, and snow are forms of precipitation, but fog
and mist are not considered precipitation because the water vapor which
constitutes them isn't dense enough to fall to the ground.
Next Topic: Rain
Weather Topic: What are Shelf Clouds?
Home - Education - Cloud Types - 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
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