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Cyclonic weather conditions resulting from the passage of cyclone 'Imelda' near the vicinity of the coast of Mauritius from the 6th to 16th of April 2013 resulted in extreme wave values recorded.
They found that cyclonic weather led to extreme surface runoff – a combination of ice melt and rain – that overwhelmed the ice sheet's basal drainage system.
In winter, cyclonic weather systems generally skirt north of the Arabian Peninsula, moving eastward from the Mediterranean Sea, though sometimes they reach eastern and central Arabia and the Persian Gulf.
The cyclonic weather system delivered heat and rain to the western edge of the Greenland ice sheet and under these warm, wet, cloudy conditions the way that the ice sheet receives energy for melt is very different to that under the more typical clear sky conditions.
The aim of this investigation was to determine the allocation between carbon dioxide concentrations, by mobile measurements at 1.5 m a.g.l., within the urban canopy layer regarding different conditions: anticyclonic and cyclonic weather situations, on weekdays, at different times of the day and in different seasons.
Bjerknes discovered that the squall line is followed by a cyclonic weather system in which air rotates around a low-pressure center.
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Observations from weather stations evidenced cyclonic rotation in the region.
Back in 1945, weather forecasters started naming cyclonic storms for recording purposes.
These zones contract to form weather fronts as the cyclonic circulation closes and intensifies.
The widespread layer clouds associated with cyclonic depressions (see below Cyclones and anticyclones), near fronts and other inclement-weather systems, are frequently composed of several layers that may extend up to 9 km (5.6 miles) or more, separated by clear zones that become filled in as rain or snow develops.
Lastly, a formative tropical cyclone needs a pre-existing system of disturbed weather, although without a circulation no cyclonic development will take place.
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