The document discusses air masses and how they influence weather patterns in North America. It defines air masses as large bodies of air with similar temperature and moisture characteristics. Air masses are classified based on their region of formation as either continental or maritime, and as either polar or tropical. Continental polar air masses are cold and dry, while maritime tropical air masses are warm and moist. The weather in eastern North America is most influenced by continental polar and maritime tropical air masses. When these air masses move over an area, they can bring significant changes in weather.
Physical Geography Lecture 08 - Precipitation, Air Masses, and Storms 110216angelaorr
The formation of precipitation. Types of precipitation. Global and U.S. precipitation. Air masses, source regions, classification. Air masses of North America. Fronts. Warm front, cold front, stationary front, occluded front. Life-cycle of a midlatitude cyclone. Weather changes with the passage of a cold front. Midlatitude anticyclones. Lightning, thunder. Tornadoes. Hurricanes. Storm surge.
Physical Geography Lecture 08 - Precipitation, Air Masses, and Storms 110216angelaorr
The formation of precipitation. Types of precipitation. Global and U.S. precipitation. Air masses, source regions, classification. Air masses of North America. Fronts. Warm front, cold front, stationary front, occluded front. Life-cycle of a midlatitude cyclone. Weather changes with the passage of a cold front. Midlatitude anticyclones. Lightning, thunder. Tornadoes. Hurricanes. Storm surge.
About air masses and it's major types with necessary image .Related course Climatology.Air mass is a volume of air defined by its temperature and water vapor content. Air
masses cover mant thousands of miles and adapt to the characteristics of the surface below them.
They are classified according to latitude and their continental or maritime source regions.
Cold air masses are termed polar or artic,while warmet air masses are deemed tropical. Continental and
superior air masses are dry while martime and monsoon air masses are moist.Weather fronts separate air
masses with different density (temperature or moisture) characteristics.An air mass may be defined as a large body of air whose physical properties especially temperature,
moisture content and lapse rate are more or less uniform horizontally for hundreds of kilometres".
According to A.N. Strahler and A.H. strahler (1978)"a body of air in which the upward gradients of
temperature and moisture are fairly uniform over a large area is known as an air mass".
Any classification of air masses must consider the fact that all of their weather characteristics (mainly
temperature, humidity and lapse rate) are properly represented and incorporated. Thus the weather
conditions of air masses at their source regions and thermodynamic and mechanical modifications
introduced in them during their journey away from their respective source regions must be taken into
definite categories.
There are two approaches to the classification of air masses.
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We all have good and bad thoughts from time to time and situation to situation. We are bombarded daily with spiraling thoughts(both negative and positive) creating all-consuming feel , making us difficult to manage with associated suffering. Good thoughts are like our Mob Signal (Positive thought) amidst noise(negative thought) in the atmosphere. Negative thoughts like noise outweigh positive thoughts. These thoughts often create unwanted confusion, trouble, stress and frustration in our mind as well as chaos in our physical world. Negative thoughts are also known as “distorted thinking”.
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Operation “Blue Star” is the only event in the history of Independent India where the state went into war with its own people. Even after about 40 years it is not clear if it was culmination of states anger over people of the region, a political game of power or start of dictatorial chapter in the democratic setup.
The people of Punjab felt alienated from main stream due to denial of their just demands during a long democratic struggle since independence. As it happen all over the word, it led to militant struggle with great loss of lives of military, police and civilian personnel. Killing of Indira Gandhi and massacre of innocent Sikhs in Delhi and other India cities was also associated with this movement.
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
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4. 20.1 Air Masses Air Masses • An air mass is an immense body of air that is characterized by similar temperatures and amounts of moisture at any given altitude. Movement of Air Masses • As it moves, the characteristics of an air mass change and so does the weather in the area over which the air mass moves. (Obj. 1) Air Masses and Weather
8. (O-2) 20.1 Air Masses Much of the weather in North America, especially weather east of the Rocky Mountains , is influenced by continental polar (cP) and maritime tropical (mT) air masses. Weather in North America
9. (O-2) Air Masses Continental Polar Air Masses • Continental polar air masses are uniformly cold and dry in winter and cool and dry in summer. Maritime Tropical Air Masses • Maritime tropical air masses are warm, loaded with moisture, and usually unstable. • Maritime tropical air is the source of much, if not most, of the precipitation received in the eastern two-thirds of the United States. Weather in North America
10. 20.1 Air Masses Maritime Polar Air Masses • Maritime polar air masses begin as cP air masses in Siberia. The cold, dry continental polar air changes into relatively mild, humid, unstable maritime polar air during its long journey across the North Pacific. • Maritime polar air masses also originate in the North Atlantic off the coast of eastern Canada. Weather in North America
13. (O-3) Air Masses Continental Tropical Air Masses • Only occasionally do cT air masses affect the weather outside their source regions. However, when a cT air mass moves from its source region in the summer, it can cause extremely hot, drought like conditions in the Great Plains. • Movements of cT air masses in the fall result in mild weather in the Great Lakes region, often called Indian summer. Weather in North America