Atmospheric Physics and Standard Atmosphere Quiz Review

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Vocabulary and concept flashcards covering atmospheric properties, pressure, temperature profiles, lapse rates, and standard atmosphere values.

Last updated 7:56 AM on 10/15/26
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10 Terms

1
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Density Altitude at 100000 Pa100000\,\text{Pa}

The density altitude measured from sea level conditions when the altimeter reads exactly 100000 Pa100000\,\text{Pa}, which is 364 ft364\,\text{ft}.

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Air Pressure at 1000 ft ASL1000\,\text{ft}\text{ ASL}

The standard atmospheric pressure at an altitude of 1000 ft1000\,\text{ft} above sea level, equal to 97.73 kPa97.73\,\text{kPa}.

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Temperature Lapse Trend

The relationship in the lower atmosphere where ambient temperature decreases as altitude increases.

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First Isothermal Layer Upper Bound

The upper boundary of the first isothermal layer in the atmosphere measured from sea level, located at an altitude of 25 km25\,\text{km}.

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Lapse Rate at 82,020.99 ft82{,}020.99\,\text{ft}

The temperature lapse rate at an altitude of 82,020.99 ft82{,}020.99\,\text{ft}, which is equal to 3×10−3 K/m3 \times 10^{-3}\,\text{K/m}.

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Stratosphere

The layer of Earth's atmosphere where commercial passenger aircraft most commonly cruise.

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Atmospheric Heights at 2.65×104 Pa2.65 \times 10^4\,\text{Pa} and 220 K220\,\text{K}

The respective altitudes corresponding to a given pressure of 2.65×104 Pa2.65 \times 10^4\,\text{Pa} and a temperature of 220 K220\,\text{K}, evaluating to 9.97 km9.97\,\text{km} and 9.85 km9.85\,\text{km}.

8
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Standard Sea-Level Pressure (lb/ft2\text{lb/ft}^2)

The standard atmospheric pressure at sea level expressed in imperial units of pounds per square foot, which equals 2116.8 lb/ft22116.8\,\text{lb/ft}^2.

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Temperature Effect on Density Altitude

The operational condition where having an ambient temperature higher than standard at a given pressure altitude causes the density altitude to increase.

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Stratospheric Pressure Variation (11–25 km11\text{--}25\,\text{km})

The mathematical function describing pressure change within the 11–25 km11\text{--}25\,\text{km} isothermal region of the stratosphere, characterized by an exponential decrease.