Why calm weather prevails in Pratip cyclonic region
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Answer:
The IMD bulletin reported that the cyclonic circulation is likely to cause widespread rainfall and thundershower along with heavy rainfall over east and adjoining parts of central India during the next 4-5 days.
The India Meteorological Department also issued a warning of isolated extremely heavy falls over Konkan during the next 24 hours and in the Gujarat region between July 4th to 6th.
The cyclone has already moved across the Lakshadweep Islands. ... On Friday, the severe cyclonic storm lay centered over eastcentral Arabian Sea about 450 km north-northwest of Aminidivi (Lakshadweep), 460 km north-northwest of Mangaluru (Karnataka) and 310 km south-southwest of Goa, IMD said in a press release.
Explanation:
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Answer:
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Explanation:
Cyclones and anti-cyclones are the primary meteorological systems that shape your weather. While anti-cyclones are associated with periods of fair weather, cyclones are responsible for shorter periods of foul weather. This foul weather ranges from overcast skies and steady rains to thunderstorms and gusty winds. When a cyclone is approaching your neck of the woods, the best course of action is to get your umbrella ready.
Cyclone Basics
The Earth features warmer temperatures near the Equator, and colder temperatures near the poles. This temperature difference creates a pressure imbalance. Pressure systems, both high and low, are nature’s regulating system that seeks to balance or equalize atmospheric pressure around the globe. Cyclones represent areas of low pressure and are, therefore, also known as low-pressure systems. They are identified on weather maps with a red “L.” Within these low-pressure systems, air rises from the surface, leading to cloud formation. As a result, low-pressure systems are associated with cloudy weather, a full-range of precipitation and strong winds.
Warm Fronts
One way that cyclones affect the weather is through their warm fronts. These fronts extend eastward from the cyclones. They represent the leading edge of warm, moist air that is moving northeastward around the cyclone’s counter clockwise circulation. As this warm air attempts to replace colder air to the north, it is gradually uplifted. This uplift forms wide layers of stratus and nimbostratus clouds. Steady rain or snow is typically encountered ahead of these warm fronts. This rainy weather generally has a long duration, due to both the slow advance of warm fronts and the shallow slope of the front itself.