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Air navigation: charts, dead reckoning and radio aids

Aviation (B.Sc Aviation; pilot / airport operations) (B.Sc Aviation) · Navigation and meteorology · free study notes for exams, placements and interviews

In short

Air navigation is the practice of fixing an aircraft's position and steering it from departure to destination within a known accuracy and time. It rests on three legs: charts (how the curved Earth is drawn on paper and how directions and distances are measured on it), dead reckoning (computing position from heading, airspeed, wind and time), and radio/satellite aids (VOR, DME, NDB, ILS, GNSS) that give independent position fixes. In India it is examined in B.Sc Aviation navigation papers and in the DGCA CPL/ATPL "Air Navigation" paper, and used daily by pilots, flight dispatchers, ATC and AAI/airline operations staff. Employers such as IndiGo, Air India, Air India Express, Akasa, AAI, Airports Authority CNS/ATM branches and ground-handling firms test exactly this material in technical rounds.

Explained

The Earth, position and direction

Charts and projections

Dead reckoning and the triangle of velocities

Ground-based radio aids

Satellite navigation, RNAV and PBN

Time, flight planning interface and units

Key points

Formulas and examples

1 NM = 1,852 m; 1 minute of latitude = 1 NM; 1° of latitude = 60 NM
Departure (NM) = ch.long (minutes of arc) × cos(latitude)
True heading/track conversions: True = Magnetic + E variation (− W variation); Magnetic = Compass + E deviation (− W deviation)
Drift = Track − Heading; Groundspeed = TAS ± wind component
Crosswind = W × sin θ; Headwind/Tailwind = W × cos θ (W = wind speed in kt, θ = angle between wind direction and runway/track)
1 in 60 rule: error angle (°) ≈ 60 × (distance off track in NM) / (distance flown in NM)
Total correction = track error angle + closing angle
Chart convergence (Lambert) = ch.long (°) × sin(parallel of origin); Earth convergency ≈ ch.long × sin(mean latitude); Conversion angle = ½ × convergency
Chart scale = chart distance / earth distance (same units); Mercator scale at latitude φ = scale at Equator × sec φ
Time = Distance / Groundspeed; TAS ≈ CAS × √(ρ0/ρ); rule of thumb TAS ≈ CAS + 2% of CAS per 1,000 ft (below about FL200)
VOR/DME theta-rho fix: position = radial (QDR) and slant range; Ground distance = √(DME range² − (height difference in NM)²)
ILS glide path height ≈ distance (NM) × 106 ft per degree of glide angle (so 3° → about 318 ft per NM)
Maximum line-of-sight range (NM) ≈ 1.23 × √(height in feet)

Example 1 - Departure and distance. Two points lie on latitude 23° N, one at 72° 30′ E (near Ahmedabad) and one at 77° 30′ E (near Bhopal).

Example 2 - Triangle of velocities (find heading and groundspeed). Desired true track 090°, TAS 150 kt, wind 180°/30 kt.

Example 3 - Compass to true and back. The compass reads 275°, deviation 2° W, variation 1° E.

Example 4 - 1 in 60 rule. An aircraft flying a 180 NM leg is found 6 NM right of track after 60 NM.

Example 5 - DME slant range and ILS height. An aircraft at 6,000 ft AMSL reads 5.0 NM DME from a station at 1,000 ft AMSL.

AidFrequency bandInformation givenTypical accuracyMain limitation
NDB / ADF190-1750 kHz (LF/MF)Bearing to station (relative)±5° or worseNight effect, static, coastal refraction
VOR / DVOR108-117.95 MHz (VHF)Magnetic radial from station±1-2°Line of sight, cone of confusion
DME960-1215 MHz (UHF)Slant range, GS, time to station±0.25 NM or 1.25%Slant-range error, limited channel pairs
ILSLOC 108-112 MHz, GP 329-335 MHzAzimuth and glide pathPrecisionNeeds protected critical areas, single approach path
GNSS + GAGANL-band (1.2-1.6 GHz)3D position, velocity, timeA few metres with SBASInterference/jamming, integrity monitoring needed
INS / IRSNone (self-contained)Position, attitude, velocityDrifts ~1-2 NM/hourDrift with time; needs alignment on ground
MercatorLambert conformal conic
Rhumb lineStraight lineCurve concave to the pole of origin
Great circleCurve concave to the EquatorNearly a straight line
ScaleExpands as sec(latitude)Nearly constant within the chart band
Convergence shownZero (meridians parallel)ch.long × sin(parallel of origin)
Best useLow latitudes, ocean plottingMid-latitude en-route and plotting charts

Where it is used

Interview questions

Common mistakes

Related topics

Aviation meteorology · Flight planning, weight and balance · Air traffic control and airspace classification · Aircraft instruments and altimetry · Avionics and communication systems · Airport operations and aeronautical information services

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