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13 Cards in this Set
- Front
- Back
State the uses of atmospheric pressure in meteorology
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- analyze typical atmospheric features
- estimate air motion - identify significant weather patterns - relate pressure to weather conditions - set aircraft altimeters for aviation 112.1.1 |
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Describe the relationship between pressure, area, and force
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p=F/A, where p=pressure, F=force, A=area
- force has direct relationship with pressure. As F grows, so proportionally will p - area has inverse relationship with pressure. As A grows, p will decrease proportionally 112.1.2 |
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State the two factors which control the surface pressure
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- change in temperature
- change in moisture content Both change density of column of air, therefore affecting mass. Heating=expansion=decreased surface pressure Cooling=contraction=increased surface pressure 112.1.3 |
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Define an isobar
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A line along which pressure is constant
112.1.4 |
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Describe the diurnal change to surface pressure
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- variations due to rhythmic expansion/contraction of atmosphere due to alternating daytime heating/nighttime cooling
- 2 pressure minima at 0400 and 1600 - 2 pressure maxima at 1000 and 2200 112.1.6 |
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State the use of pressure levels in meteorology
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- displays the state of atmosphere at specific levles of pressure altitude
- upper air charts depict height variations above MSL and height patterns - analysis provides info pursuant to safety and efficiency of flight ops 112.2.1 |
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Define the hydrostatic equilibrium
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- exists in atmosphere when vertical component of Pressure Gradient Force at any given level is in exact balance with force of gravity at that level
112.2.2 |
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Describe the relationship between the thickness of an atmospheric layer, the density of the air, and the average temperature
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Thickness increases if temp increases:
- warm air less dense, expands, and thicker layer - cold air more dense, compresses, and thinner layer 112.2.3 |
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State the two factors which affect the height of a pressure level
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- value of MSL
- mean temp of column of air beneath the pressure level 112.2.4 |
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Given a variation in one of the two factors which affect the height of a pressure level, state its effect
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- height of pressure level higher when MSL pressure higher and/or column temps higher
- height of pressure level lower when MSL pressure lower and/or column temps lower 112.2.5 |
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Given a diagram depicting the vertical variations of pressure levels identify a cold high, cold low, warm low, and warm high
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Cold high:
- high surface pressure and upper level lower pressure Cold low: - low surface pressure and upper level lower pressure Warm low: - low surface pressure and upper level high pressure Warm high: - high surface pressure and upper level high pressure 112.2.6 |
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Explain the seasonal variations in the height of a pressure level in mid latitude
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In winter, average pressure height in troposphere becomes lower because mean temp in the troposphere becomes colder
112.2.7 |
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Explain the variation in the height of a pressure level from Pole to the Equator
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Since temps get warmer approaching the equator, and pressure level height directly linked to temps, height of pressure levels rise as you proceed from Pole to the equator
112.2.8 |