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01.11.2014

What is a depression weather, tinnitus zen - .

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Viewed from above, the air within a depression circulates in an anti-clockwise direction in the Northern hemisphere (they circulate clockwise in the Southern hemisphere). A high pressure system, also known as an anticyclone occurs when the weather is dominated by stable conditions.
Anticyclones can be identified on weather charts as an often large area of widely spaced isobars, where pressure is higher than surrounding areas.
A low pressure system, also known as a depression occurs when the weather is dominated by unstable conditions. Depressions can be identified on weather charts as an area of closely spaced isobars, often in a roughly circular shape, where pressure is lower than surrounding areas.
The diagram below shows a cross section through a warm front, with associated cloud, temperature and weather changes. The diagram below shows a cross section through a cold front, with associated cloud, temperature and weather changes.


A Norwegian scientist called Vilhelm Bjerknes devised a simple model which described how depressions developed from the meeting of warm and cold air.
Most depressions have a warm and cold front, more mature depressions may also have an occluded front.
Using this information on the passage of depressions you should now be able to complete worksheet 3, and worksheet 4.
The weather is normally dry, although occasionally, very hot temperatures can trigger thunderstorms. The diagram below shows a cross-section through a depression, showing the warm and cold fronts and an indication of the associated weather. Because of these stable conditions, cloud formation is inhibited, so the weather is usually settled with only small amounts of cloud cover.
This rising air cools and condenses and helps encourage cloud formation, so the weather is often cloudy and wet.


The passage of weather associated with a cold front is much shorter lived than that with a warm front.
The weather ahead of an occlusion is similar to that ahead of a warm front, whilst the weather behind is similar to that behind a cold front.
As this part of the depression passes over, there may be a short period of clear, dry weather. However, at the trailing cold front, heavier, cooler air meets the warm air at the centre of the depression, undercutting it and forcing it steeply upwards.




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