Joseph R. Badick - Flight Theory and Aerodynamics

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FLIGHT THEORY
AERODYNAMICS
GET A PILOT’S PERSPECTIVE ON FLIGHT AERODYNAMICS FROM THE MOST UP-TO-DATE EDITION OF A CLASSIC TEXT Flight Theory and Aerodynamics
Flight Theory and Aerodynamics
Flight Theory and Aerodynamics

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ICAO STANDARD ATMOSPHERE

To provide a basis for comparing aircraft performance at different parts of the world and under varying atmospheric conditions, the performance data must be reduced to a set of standard conditions. These are defined by the International Civil Aviation Organization (ICAO) and are compiled in a standard atmosphere table. An abbreviated table is shown here as Table 2.1. Columns in the table show standard day density, density ratio, pressure, pressure ratio, temperature, temperature ratio, and speed of sound at various altitudes.

Table 2.1Standard atmosphere table

Altitude (ft) Density ratio, σ картинка 59 Pressure ratio, δ Temperature (°F) Temperature ratio, θ Speed of sound (kts.) Kinematic viscosity, v (ft 2/s)
0 1.0000 1.0000 1.0000 59.00 1.0000 661.7 0.000 158
1 000 0.9711 0.9854 0.9644 55.43 0.9931 659.5 0.000 161
2 000 0.9428 0.9710 0.9298 51.87 0.9862 657.2 0.000 165
3 000 0.9151 0.9566 0.8962 48.30 0.9794 654.9 0.000 169
4 000 0.8881 0.9424 0.8637 44.74 0.9725 652.6 0.000 174
5 000 0.8617 0.9283 0.8320 41.17 0.9656 650.3 0.000 178
6 000 0.8359 0.9143 0.8014 37.60 0.9587 647.9 0.000 182
7 000 0.8106 0.9004 0.7716 34.04 0.9519 645.6 0.000 187
8 000 0.7860 0.8866 0.7428 30.47 0.9450 643.3 0.000 192
9 000 0.7620 0.8729 0.7148 26.90 0.9381 640.9 0.000 197
10 000 0.7385 0.8593 0.6877 23.34 0.9312 638.6 0.000 202
15 000 0.6292 0.7932 0.5643 5.51 0.8969 626.7 0.000 229
20 000 0.5328 0.7299 0.4595 −12.32 0.8625 614.6 0.000 262
25 000 0.4481 0.6694 0.3711 −30.15 0.8281 602.2 0.000 302
30 000 0.3741 0.6117 0.2970 −47.98 0.7937 589.5 0.000 349
35 000 0.3099 0.5567 0.2353 −65.82 0.7594 576.6 0.000 405
36 089 a 0.2971 0.5450 0.2234 −69.70 0.7519 573.8 0.000 419
40 000 0.2462 0.4962 0.1851 −69.70 0.7519 573.8 0.000 506
45 000 0.1936 0.4400 0.1455 −69.70 0.7519 573.8 0.000 643
50 000 0.1522 0.3002 0.1145 −69.70 0.7519 573.8 0.000 818

aThe tropopause.

ALTITUDE MEASUREMENT

When a pilot uses the term altitude, the reference is usually to altitude above sea level as read on the altimeter, but it is important that the distinction is made to understand what types of altitude exist. When meteorologists refer to the height of the cloud layer above an airfield, they are usually referring to the altitude above the field elevation. When air traffic control refers to an altitude at FL180 and above, they are referring to pressure altitude. A flight crew in an aircraft approaching the runway during a low ceiling CAT III instrument approach will need to understand the value of a radar altimeter. Understanding what “altitudes” are important at different periods of flight, and the effect of temperature, pressure, and moisture on those altitudes, is imperative for safe flight.

Indicated Altitude

Indicated altitude is the altitude that is read directly from the altimeter and is uncorrected for any errors. In the United States, below FL180 the altimeter is set to the current altimeter setting of the field you are departing from or arriving to, or is given by air traffic control for the current area you are flying in. In the United States, when flying at or above 18 000 ft, altitude is measured in Flight Levels (e.g. FL180 for 18 000 ft). At FL180, the indicated altitude will be equal to pressure altitude as the altimeter setting is set to 29.92″, standard pressure, or QNE. The altitude at which the crew changes to 29.92 is called the transition altitude (TA). When the crew descends for landing, the altitude at which they return the altimeter setting to local barometric pressure corrected to sea level (QNH) is called the transition level (TL). (Remember it this way: 29.92 is selected at the TA, and the “A” stands for aloft, as in climbing or cruise. When returning to land, the TL is set on descent, and “L” stands for low, or landing.)

When QNE is lower than 29.92, the lowest usable flight level is no longer FL180. The lowest usable FL is obtained from the aeronautical publications. For instance, in the United States, if the pressure in the area of operations is between 29.91 and 29.42″, the lowest usable enroute altitude is FL185. It should also be noted that the TA and TL outside the United States will not always be 18 000. ICAO members set their own values.

Incidentally, QFE is the reference pressure set in the altimeter if the pilot wishes to know the elevation above the airfield. When the aircraft is on the airfield, the altimeter reads zero. QFE is seldom used as it would be of limited value when away from the immediate vicinity of the airfield.

Calibrated Altitude

Calibrated altitude is indicated altitude corrected for instrument and installation errors.

True Altitude

True altitude is the actual altitude above mean sea level and is referenced as mean sea level (MSL). On most aeronautical charts, MSL altitudes are published for man‐made objects such as towers and buildings, as well as for terrain, since this is the altitude closest to the altitude read off the altimeter. An important note is that true altitude will only be the same as indicated altitude when flying in standard conditions, which is very rare. When flying in conditions colder than standard, the altimeter will indicate a higher altitude then you are flying, so true altitude will be lower than indicated altitude. The same dangerous situation can develop when you are flying from a high‐pressure area to a low‐pressure area and the altimeter is not corrected for the local altimeter setting. Your altimeter will interpret the lower pressure as a higher altitude and your true altitude will again be lower than your indicated altitude. From the variations in true altitude versus indicated altitude, the saying was developed “high to low, or hot to cold, look out below.” Of course, this assumes that the altimeter is never reset to local pressure for an entire flight covering a long distance with varying temperatures and pressures.

Absolute Altitude

Absolute altitude is the vertical altitude above the ground (AGL), and can be measured with devices like a radar altimeter. Of course, your absolute altitude is more critical the closer to the ground you are flying; so even when not equipped with a radar altimeter, a pilot should be aware of their AGL altitude. When conducting an instrument approach in inclement weather, knowledge of your AGL altitude is vital to the safe completion of the approach or execution of a missed approach. Your height above airport (HAA), height above touchdown zone (HAT), and decision height (DH) are all AGL altitudes and should be briefed before the approach.

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