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旋翼機飛行手冊 ROTORCRAFT FLYING HANDBOOK

時間:2011-04-05 11:32來源:藍天飛行翻譯 作者:航空 點擊:

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MAGNETIC COMPASS
In some helicopters, the magnetic compass is the only direction seeking instrument. Although the compass appears to move, it is actually mounted in such a way that the helicopter turns about the compass card as the card maintains its alignment with magnetic north.
COMPASS ERRORS
The magnetic compass can only give you reliable directional information if you understand its limitations and inherent errors. These include magnetic variation, compass deviation, and magnetic dip.
MAGNETIC VARIATION
When you fly under visual flight rules, you ordinarily navigate by referring to charts, which are oriented to true north. Because the aircraft compass is oriented to magnetic north, you must make allowances for the difference between these poles in order to navigate properly. You do this by applying a correction called variation to convert a true direction to a magnet direction. Variation at a given point is the angular difference between the true and magnetic poles. The amount of variation depends on where you are located on the earth’s surface. Isogonic lines connect points where the variation is equal, while the agonic line defines the points where the variation is zero. [Figure 12-9] 

 

 

COMPASS DEVIATION
Besides the magnetic fields generated by the earth, other magnetic fields are produced by metal and electrical accessories within the helicopter. These magnetic fields distort the earth’s magnet force and cause the compass to swing away from the correct heading. Manufacturers often install compensating magnets within the compass housing to reduce the effects of deviation. These magnets are usually adjusted while the engine is running and all electrical equipment is operating. Deviation error, however, cannot be completely eliminated; therefore, a compass correction card is mounted near the compass. The compass correction card corrects for deviation that occurs from one heading to the next as the lines of force interact at different angles.
MAGNETIC DIP
Magnetic dip is the result of the vertical component of the earth’s magnetic field. This dip is virtually nonexistent at the magnetic equator, since the lines of force are parallel to the earth’s surface and the vertical component is minimal. As you move a compass toward the poles, the vertical component increases, and magnetic dip becomes more apparent at these higher latitudes.
Magnetic dip is responsible for compass errors during acceleration, deceleration, and turns.
Acceleration and deceleration errors are fluctuations in the compass during changes in speed. In the northern hemisphere, the compass swings toward the north during acceleration and toward the south during deceleration. When the speed stabilizes, the compass returns to an accurate indication. This error is most pronounced when you are flying on a heading of east or west, and decreases gradually as you fly closer to a north or south heading. The error does not occur when you are flying directly north or south. The memory aid, ANDS (Accelerate North, Decelerate South) may help you recall this error. In the southern hemisphere, this error occurs in the opposite direction.

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