Atmosphere Flashcards
Radius of the Earth
Polar radius of 3432NM
Equatorial radius of 3444NM
What’s a Great Circle?
circle on the surface of the Earth with the same centre and the same radius as the Earth itself
Rhomb Lines
lines on the surface of the Earth, which crosses the meridians at a constant angle
*flights under 1000NM usually fly along this track
Standard Pressure at MSL
1013.25 hPa
Decreases at 1 hPa per 27’
Standard Temperature at SL
15° C
Decrease at a rate of 1.98° per 1000’
Boyle’s Law
At constant temperature, as the pressure of gas increases, its volume must decrease
Charles Law
At constant pressure, if temperature increases, gas expands (volume increases)
Density Altitude
Pressure altitude corrected for non standard temperature
DA = PA + (ISA Deviation x 120)
Relative Humidity
- Amount of moisture in the air compared to the total amount that can be present at that temperature
- warm air can contain more moisture than cold air
Dew point
Temperature at which air reaches a state where it can hold no more water
Average Environmental Lapse Rate (ELR)/Saturated Adiabatic Lapse Rate (SALR)
1.8°C/1000’ or 0.6°C/100 m
Dry Adiabatic Lapse Rate
3°C/1000’ or 1°C/100 m
Dew point lapse rate
0.5°C/1000 ft
Layers of the Atmosphere
Troposphere - surface to 11km above (36,000’)
Stratosphere - to 50km (31 miles)
Mesosphere - to 85km (53 miles)
Thermosphere - to 690km (430 miles)
Exosphere - to 10,000 km
Importance of Tropopause
- Boundary layer of Troposphere
- traps moisture and associated weather in the Troposphere
- varies with latitude and seasons of the year
- associated with the Jet stream and Clear Air Turbulence (CAT)
- lower in the winter and higher in the summer
- lower at the poles and higher at the equator
- avg of 36,000’ (11 km) at 45º latitude