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Jet Stream
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When watching the evening weather report, chances are good you will hear something about the jet stream This speedy current is commonly thousands of kilometers long, a few hundred kilometers wide, and only a few kilometers thick Jet streams are found between 10 to 14 km above the Earth s surface in the troposphere Blowing from west to east at speeds of 240 km/h, they can also dip northward or southward depending on atmospheric conditions The jet stream is a long, narrow current of fast moving air found in the upper atmospheric levels Air temperature differences drive the jet stream The bigger the temperature differences, the stronger the pressure differences between warm and cold air Strong pressure differences create strong winds This is why jet streams fluctuate so much in speed During the winter months, polar and equatorial air masses form a sharp surface temperature contrast causing an intense jet stream The strong jet stream pushes farther south
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Cold deserts 60 N Temperate zone 30 N Westerlies Hot deserts Northeast trade winds
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Equator Southeast trade winds
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Figure 62 Trade winds are found at certain latitudes or regions on the Earth in the winter However, during the summer months, when the surface temperature difference is less severe, jet stream winds are weaker The jet stream then moves farther north
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Wind Chill
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Wind chill factor measures the rate of heat loss from exposed skin to that of surrounding air temperatures
Wind chill occurs when winter winds cool objects down to the temperature of the surrounding area; the stronger the wind, the faster the rate of cooling For example, the human body is usually around 36 C in temperature, a lot higher than a cool Montana day in November Our body s heat loss is controlled by a thin insulating layer of warm air held in place above the skin s surface by friction If there is no wind, the layer is undisturbed and we feel comfortable However, if a wind gust sweeps this insulating layer of air away, we feel Table 61 Wind chill can bring down the temperature of the body quickly
15 C 15 TEMPERATURE ( C) 10 C 5 C 0 C 10 5 0 5 C 5 10 C 10 15 C 15 20 C 20
Wind speed (km/h)
0 5 10 30 50 70 90
18 20 24 29 35 41
13 14 18 21 24 30
7 8 12 14 15 19
2 3 6 7 8 9
3 2 1 0 1 2
9 8 7 6 6 5
14 13 12 12 12 12
19 19 18 18 18 18
Atmospheric Composition 61
chilled The protective air layer must be reheated by the body See Table 61 to get an idea of the wind chill equivalent temperatures at different wind speeds
Air Pressure
Bakers living in the mountains have to consider air pressure when creating light cakes and souffl s Lower pressure at high altitudes (over 6,000 km) changes the baking process from that of sea-level baking In fact, cake mixes give different directions for high-altitude baking to make up for the pressure difference on the rising cake
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Air pressure is the force applied on you by the weight of air molecules Although air is invisible, it still has weight and takes up space Free-floating air molecules are pressurized when crowded into a small volume The downward force of gravity gives the atmosphere a pressure or a force per unit area The Earth s atmosphere presses down on every surface with a force of 1 kilogram (kg) per square centimeter The force on 1,000 cm2 is nearly a ton! Weather scientists measure air pressure with a barometer Barometers measure air pressure in centimeters of mercury or millibars A measurement of 760 mm of mercury is equal to 101325 millibars Air pressure tells us a lot about the weather With a high-pressure system, there are cooler temperatures and sunny skies When a low-pressure system moves in, look for warmer temperatures and thunderstorms Atmospheric pressure falls with increasing altitude A pillar of air in cross section, measured from sea level to the top of the atmosphere, weighs approximately 147 pounds per square inch (psi) Atmospheric pressure (atm) at sea level is equal to 1 atm = 760 mmHg (millimeters of mercury) = 1013 millibars = 147 psi = 101325 hPa (hectopascals) On weather maps, changes in atmospheric pressure are shown by lines called isobars An isobar is a line connecting areas of the same atmospheric pressure It s very similar to the lines connecting equal elevations on a topographical map
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