Description of weather patterns

        Air mint are how weather travels through proscribed the world and the

weather creates weather patterns.Air masses and accompanying fronts do not

remain nonmoving for long. Although their movements are never exactly the

same, they do exhibit few patterns that help meteorologists and others predict

the weather. The enclosure between devil air masses is called a front. As a result,

moving fronts indicate a transplant in the weather. The fronts are moved in things

called Jet Streams On a weather map fronts are drawn where at that place is a large

change in temperature and a shift in nullity direction. A front can also be

described as the boundary between adjacent Highs with different conditions.

        Meteorologists often call temper patterns oscillations, since they

change on time scales ranging from days to decades. Interactions between the

atmosphere and the oceans are at the core of most of the patterns. The

atmosphere and ocean push and pull against angiotensin-converting enzyme another. When one does

something, it affects the other. Since the ocean is much slower to respond to

environmental changes than the atmosphere, the two players are unequal

partners.

        

        Jet streams are bands of very strong winds which pass at limited

altitudes usually in the 30-40000 feet area.



They can be over 150 miles wide and

1000 miles long and can travel at over 250 mph. Like most winds they occur

where there is a deflexion between hot and nippy, and in the commons streams case

this means close to the joins of tropical and polar air The jet stream is a river of

fast flowing air at high altitudes above the demesne that generally flows from west to

east over the mid-latitudes.To be called a jet stream the winds should be faster

than 57 mph. Usually, the jet stream separates cold polar air to...

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