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The Norwegian Cyclone Model is an idealized formation model of cold-core cyclonic storms developed by Norwegian meteorologists during the First World War.
From October to March, prevailing westerly winds bring cyclonic storms and rains across northern Libya.
In the western valleys, convectional storms, in combination with cyclonic storms, are common in the summer.
The Northern Rockies tend to receive precipitation more evenly throughout the year from Pacific cyclonic storms.
It flows only after exceptional cyclonic storms ("willy-willies") and may be several miles wide during high flood.
Cyclonic storms form and move eastward through the zone where the temperate and tropical air masses are in contact, called the polar front, which shifts southward in winter.
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Elsewhere this is called a tropical cyclone, severe tropical cyclone, or severe cyclonic storm.
The 2002 Oman cyclone (JTWC designation: 01A, officially known as Cyclonic Storm ARB 01 ) was an uncommon tropical cyclone that struck the Dhofar region of Oman in May 2002.
L. S. Rathore, director general of the India Meteorological Department, termed the storm, named Cyclone Phailin, a "very serious cyclonic storm".
In May 2003, a tropical cyclone known as Very Severe Cyclonic Storm BOB 01 produced the worst flooding in Sri Lanka in 56 years.
At this time, the IMD classified the cyclone as a Very Severe Cyclonic Storm and reported that it had a 60 km wide eye.
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