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{"id":193318,"date":"2021-12-28T20:58:19","date_gmt":"2021-12-28T20:58:19","guid":{"rendered":"https:\/\/nursingwritershelp.com\/?p=193318"},"modified":"2021-12-28T20:58:19","modified_gmt":"2021-12-28T20:58:19","slug":"air-masses-fronts-weather-maps","status":"publish","type":"post","link":"https:\/\/nursingwritershelp.com\/air-masses-fronts-weather-maps\/","title":{"rendered":"Air Masses, Fronts, Weather Maps"},"content":{"rendered":"<\/p>\nAir masses<\/strong> are large bodies of air (over 1,000 miles in diameter) that possess similar<\/p>\n<\/strong><\/p>\ntemperature and moisture characteristics throughout. An air mass acquires these characteristics above an area of land or water known as its source region. When the air mass sits over a region for several days, or longer, it picks up the distinct temperature and humidity characteristics of that region.<\/p>\n
The basic types of air masses are: maritime tropical (mT), continental tropical (cT), maritime polar (mP), continental polar (cP), and continental arctic (cA).<\/strong> <\/p>\nA front<\/strong> is the area along which two different air masses meet. At a front, the two air masses have different densities, based on temperature, and do not easily mix. One air mass is lifted above the other, creating a low pressure zone. If the lifted air is moist, there will be condensation and precipitation. Winds are common at a front. The greater the temperature difference between the two air masses, the stronger the winds will be. Fronts are the main cause of stormy weather. <\/p>\nAlong a cold front<\/strong>, the denser, cold air pushes up the warm air, causing the air pressure to decrease. At the front, there will be a line of rain showers, snow showers, or thunderstorms with blustery winds. Along a warm front<\/strong>, a warm air mass slides over a cold air mass. When warm, less dense air moves over the colder, denser air, the atmosphere is relatively stable.<\/p>\n<\/p><\/p>\n \n