Mature midlatitude

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After completing this section, you should be able to discuss the ingredients needed for a mid-latitude cyclone to form and thrive. You should also be able to discuss the resulting temperature advections caused by a mid-latitude cyclone's circulation, define the warm sector, and discuss the conditions that bring about the demise of a mid-latitude cyclone. Some low-pressure systems become legendary.

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At the completion of this section, you should be able to name the three conveyor belts associated with a mature mid-latitude cyclone. You should also be able to describe each conveyor belt and discuss its impacts on the mid-latitude cyclone precipitation, appearance, etc. One of the common characteristics of mid-latitude cyclones is their distinctive appearance on radar and satellite imagery.

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We often hear the terms high pressure and low pressure in weather reports. Low pressure means that the atmospheric pressure of a region is lower than the surrounding area; when the situation is reversed, it is called high pressure. Therefore, the designation of high and low pressure is only relative like the designation of peaks and valleys in mountainous areas.

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Mid-latitude or frontal cyclones are large traveling atmospheric cyclonic storms up to kilometers in diameter with centers of low atmospheric pressure. An intense mid-latitude cyclone may have a surface pressure as low as millibars, compared to an average sea-level pressure of millibars. Normally, individual frontal cyclones exist for about 3 to 10 days moving in a generally west to east direction.

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Air masses are large bodies of air that share uniform temperature and moisture characteristics. These air masses develop over large areas with stable weather and pick up the characteristics of the surface beneath them. We classify the air masses depending upon whether they have developed over water or land and whether over polar or tropical regions.

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Take one letter from the temperature group and one from the moisture group to define an air mass. Lower case moisture is written first followed by the upper case temperature letter. Example: cP - continental polar - cold and dry. Pacific air mass affects the U.

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