MadSci Network: Earth Sciences |
There is no hard and fast rule for which is more dominant feature affecting weather on a daily basis. Fronts are boundaries marking the transition zone between air masses. If the air masses have vastly different characteristics (temperature and moisture content), then the boundary between them is very distinct. If the air masses are fairly similar, then the front marking the boundary between them can be very indistinct. Typically, an area of low pressure has a warm front emanating from the center of the low toward the east and a cold front emanating from its center toward the south or southwest. Well behind (west of) the cold front will be a high pressure center while another area of high pressure will be well ahead (east of) the area of low pressure. However, as boundaries between differing air masses fronts can form without accompanying areas of low pressure. Sometimes, southerly flow on the west side of an area of high pressure will result in the formation of a warm front. Other times, north to northwest winds east of an area of high pressure will result in cold frontal formation. The processes involved in frontal and cyclone formation are extremely complicated. Good summary information can be found in many different books written for the layman. Your local bookstore or library should have several. Some examples include: The Weather Book (by Jack Williams of USA Today), The National Audubon Society Field Guide to North American Weather, Weather (A Golden Guide), and A Field Guide to the Atmosphere (Peterson Field Guide).
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