A Great Circle is a circle on the surface of the Earth whose centre and radius are those of the Earth itself. It is called "great" because a disc cut in the plane of the Great Circle would have the largest area achievable — it divides the Earth into two equal hemispheres.
Key properties:
A Rhumb Line is a regularly curved line on the surface of the Earth that cuts all meridians at the same angle — a line of constant direction.
The constant-direction property was enormously important to mariners and early aviators, who navigated by compass heading along straight Mercator chart tracks. Unlike the Great Circle, the Rhumb Line is not the shortest distance (except along the Equator, a meridian, or a parallel of latitude).
The Great Circle is always the shorter path; the Rhumb Line is always the longer one (again, except for the special cases — Equator, meridians).
There is only one Rhumb Line between any two points.
The only lines that are simultaneously Great Circles AND Rhumb Lines are:
Note: Parallels of latitude (other than the Equator) are Rhumb Lines but are Small Circles — their plane does not pass through the Earth's centre.
Because a Great Circle track curves toward the nearer Pole, its direction changes continuously. The pattern of this change is captured in the DIID rule.
Consider an East–West Rhumb Line track (090° or 270°) at ~50°N or ~50°S:
| Hemisphere | Going East (→) | Going West (←) |
|---|---|---|
| Northern | GC track starts high (030°), swings to 090°, finishes low (150°) — track angle INCREASING | GC track starts low (330°), swings to 270°, finishes high (210°) — track angle DECREASING |
| Southern | GC track starts low (150°), swings to 090°, finishes high (030°) — track angle DECREASING | GC track starts high (210°), swings to 270°, finishes low (330°) — track angle INCREASING |
Reading the four quadrants clockwise from the top-left: D–I–I–D (Decreasing–Increasing–Increasing–Decreasing).
In ALL cases: the GC direction always changes towards the Equator.
| Unit | Equivalent |
|---|---|
| 1 metre (m) | 100 cm = 1 000 mm |
| 1 kilometre (km) | 1/10 000th of Equator-to-Pole distance → Earth circumference = 40 000 km |
| 1 km | 3 280 ft |
| 1 m | 3.28 ft |
| Unit | Equivalent |
|---|---|
| 1 foot (ft) | 12 inches |
| 1 yard (yd) | 3 feet |
| 1 inch | 2.54 cm |
| 1 statute mile | 5 280 ft |
The nautical mile is directly related to the Earth's angular measurements:
| Angular Measurement | Distance |
|---|---|
| 1° of latitude | 60 NM |
| Equator to either Pole (90°) | 5 400 NM |
| Earth circumference (360°) | 21 600 NM |
The full definition: the NM is the arc of a Great Circle that subtends 1 minute of arc at the centre of curvature. Because the Earth is an oblate spheroid, the radius of curvature varies with latitude:
| Location | Radius of curvature | NM length |
|---|---|---|
| Equator | Smallest (most curved) | ~6 048 ft (shortest) |
| Standard (mean) | Mean | 6 076.1 ft (International NM = 1 852 m) |
| Poles | Largest (flattest) | ~6 108 ft (longest) |
For all DGCA exam calculations, use the Standard NM of 6 080 ft. The variation between 6 048 ft and 6 108 ft is not examined computationally — it is a conceptual understanding question only.
| Conversion | Value |
|---|---|
| 5 400 NM = | 10 000 km |
| 21 600 NM = | 40 000 km |
| 1 NM = | 1 852 m = 6 080 ft |
| 1 km = | 3 280 ft |
| 1 km = | 0.5400 NM (= 5400/10000) |
| 1 NM = | 1.852 km |
Use the circumference ratio: 21 600 NM = 40 000 km.
Therefore: NM × (40 000/21 600) = km | km × (21 600/40 000) = NM
Or simply: NM × 1.852 = km | km ÷ 1.852 = NM
General GC distance calculation requires spherical geometry — not in the DGCA syllabus. Exam questions are limited to points on special Great Circles: the same meridian, meridian & anti-meridian, or the Equator. There are five general cases plus a special antipodal case — all six are shown below.
| Condition | Case |
|---|---|
| Same longitude, same hemisphere | Case 1 — Ch.lat direct |
| Same longitude, different hemispheres | Case 2 — Ch.lat = sum of lats |
| Longitudes add to 180°, same hemisphere | Case 3 — Route via nearer Pole |
| Longitudes add to 180°, different hemispheres | Case 4 — Route via nearer Pole |
| Both at 0° latitude (Equator) | Case 5 — Ch.long at Equator |
| Same lat N & S, lons add to 180° | Case 6 — Antipodal (10 800 NM) |
If your angular distance exceeds 180°, you've gone the wrong way around. Subtract from 360° for the angular answer, or subtract from 21 600 NM for the distance.
The conversion 1 minute of longitude = 1 NM is valid ONLY AT THE EQUATOR. At any other latitude, you must use the departure formula (covered in the Departure chapter).
The mean latitude between two positions is their arithmetic average. It is used in departure calculations (Ch.15).
Example 1 — same hemisphere: Mean lat of 52°17'N and 17°57'N
52°17' + 17°57' = 70°14' ÷ 2 = 35°07'N
Example 2 — different hemispheres: Mean lat of 35°25'N and 13°38'S
Total span = 35°25' + 13°38' = 49°03'. Half = 24°31.5'.
Mean lat = 35°25'N − 24°31.5' = 10°53.5'N
11 questions (many with sub-parts) • Calculation, conceptual & MCQ • Full worked solutions
| Part | Calculation | Answer |
|---|---|---|
| (a) | 52°15' − 39°35' = 12°40' South | 12°40'S |
| (b) | 49°35'N + 60°20'S (cross Equator) = 109°55' South | 109°55'S |
| (c) | 74°20'S → 34°30'S: 74°20' − 34°30' = 39°50' North | 39°50'N |
| (d) | 71°20'N→Pole: 18°40' + Pole→86°45'N: 3°15' = 21°55' | 21°55' |
Part (b) note: When crossing the Equator, add both latitudes (49°35' + 60°20' = 109°55').
Part (c) note: Both in Southern hemisphere — the aircraft travels northward (toward less southerly latitude). Subtract the smaller from the larger: 74°20' − 34°30' = 39°50'N.
Part (d) note: "Over the North Pole" means the route passes through 90°N and continues on the opposite meridian. From 71°20'N to the pole = 18°40'; pole to 86°45'N = 3°15'. Total = 21°55'.
Step 1 — Ch.lat: 79°30' − 41°25' = 38°05'N
Step 2 — NM: (38 × 60) + 5 = 2 285 NM
Step 3 — km: 2 285 × 1.852 = 4 232 km (or 4 230 km using the nav computer)
| Part | Calculation | Answer |
|---|---|---|
| (a) | 125°35' − 075°40' = 49°55' West (same side) | 49°55'W |
| (b) | 001°20' + 004°20' = 05°40' West (opposite sides) | 05°40'W |
| (c) | 179°30' − 150°40' = 28°50' East (same side) | 28°50'E |
| (d) | 162°36' + 140°42' = 303°18' → shorter arc: 360° − 303°18' = 56°42'W | 56°42'W |
Rule: same side → subtract; opposite sides → add. If the result exceeds 180°, take the supplement (360° − result) — this is the shorter arc.
Part (d) detailed: 162°36'W and 140°42'E are on opposite sides, so add: 162°36' + 140°42' = 303°18'. Since 303°18' > 180°, the shorter arc is 360° − 303°18' = 56°42'. Going westward from 162°36'W by 56°42' takes you through the anti-meridian to 140°42'E.
| Part | Ch.lat | Ch.long |
|---|---|---|
| (a) | 01°29'N | 002°05'W |
| (b) | 03°36'S | 001°13'E |
| (c) | 00°26'N | 005°22'E |
| (d) | 67°24'N | 004°44'E |
| (e) | 00°01'N | 014°36'E |
(a) Lat: 52°00' − 50°31' = 01°29'N. Long: 008°35'W − 006°30'W = 002°05'W (going further west).
(b) Lat: 43°56' − 47°32' = 03°36'S (going south). Long: 002°46'W → 001°33'W = 001°13'E (going east, less westerly).
(c) Lat: 62°13' − 61°47' = 00°26'N. Long: 003°46'W + 001°36'E = 005°22'E (crossing prime meridian).
(d) Lat: 35°57'N + 31°27'S = 67°24'N (cross Equator northbound). Long: 096°31' − 091°47' = 004°44'E.
(e) Lat: 51°06' − 51°05' = 00°01'N. Long: 177°42'E → 167°42'W — going east: 177°42'E to 180° = 2°18', then 180° to 167°42'W = 12°18'. Total = 014°36'E (shorter arc eastward).
| Part | Case | NM | km |
|---|---|---|---|
| (a) | Case 1 (same meridian, same hemi) | 90 NM | 167 km |
| (b) | Case 2 (same meridian, diff hemi) | 482 NM | 893 km |
| (c) | Case 3 (merid+anti-merid, same hemi) | 3 360 NM | 6 223 km |
| (d) | Case 5 (Equator) | 660 NM | 1 222 km |
| (e) | Case 6 (Antipodal) | 10 800 NM | 20 000 km |
(a) Same lon 002°32'E. Ch.lat = 53°36' − 52°06' = 01°30' = 90 NM. × 1.852 = 167 km.
(b) Same lon 163°36'W. Ch.lat = 04°41' + 03°21' = 08°02' = 482 NM. × 1.852 = 893 km.
(c) 093°00'E + 087°00'W = 180° → Case 3. Both 62°N → route over N Pole. Angular = 180° − (62° + 62°) = 56° = 3 360 NM. × 1.852 = 6 223 km.
(d) Both on Equator → Case 5. Ch.long: 176°E + 173°W = 349°; shorter arc = 360° − 349° = 11°. At Equator: 11° × 60 = 660 NM. × 1.852 = 1 222 km.
(e) 071°37'W + 108°23'E = 180° AND equal lats N/S → Antipodal (Case 6). Distance = 180° = 10 800 NM = 20 000 km.
(a) Initial track: 360°(T) — True North
(b) Track changes: No
(c) Route is over the North Pole. Initial track is True North; once past the pole, the track becomes True South (180°T).
Step 1 — Identify case: 002°30'E + 177°30'W = 180° → meridian/anti-meridian. Both at 72°N → same hemisphere → Case 3 (route over North Pole).
Step 2 — Initial direction: From 72°N heading to the North Pole = due North = 360°(T).
Step 3 — Track consistency: As the aircraft crosses the pole, "north" flips to "south" on the Mercator representation. The track direction changes from 360°T to 180°T — so No, it does not remain constant.
Latitude: 54°20'N + 16°20'N = 70°40'N
Longitude: 002°30'W + 20°30'W = 023°00'W
Latitude: 36°47'S + 46°47'N (northward change crosses Equator): 46°47' − 36°47' = 10°00'N
Longitude: 179°21'E + 20°30'E = 199°51'E. Since > 180°: 360° − 199°51' = 160°09'W
(a) Northern hemisphere: Rhumb Line is nearer the Equator (South of the Great Circle)
(b) Southern hemisphere: Rhumb Line is nearer the Equator (North of the Great Circle)
In both hemispheres, the Rhumb Line lies nearer to the Equator, while the Great Circle bulges toward the nearer Pole. This is why the GC is the shorter path — it cuts across the "top" of the curved path rather than staying at the lower latitude.
A meridian is simultaneously both:
Cutting all meridians at the same angle is equivalent to maintaining a constant compass direction. This is the defining property of a Rhumb Line and the basis of traditional compass navigation.
| Parameter | Value | Section |
|---|---|---|
| 1 NM (ICAO) | 1 852 m | §5 |
| 1 NM (Standard/Admiralty) | 6 080 ft | §5 |
| 1 NM (at Equator) | ~6 048 ft (shortest) | §6 |
| 1 NM (International mean) | 6 076.1 ft | §6 |
| 1 NM (at Poles) | ~6 108 ft (longest) | §6 |
| Earth circumference | 21 600 NM = 40 000 km | §7 |
| Equator to Pole | 5 400 NM = 10 000 km | §7 |
| 1 km | 3 280 ft = 0.5400 NM | §7 |
| 1 m | 3.28 ft | §5 |
| 1 inch | 2.54 cm | §5 |
| 1 statute mile | 5 280 ft | §5 |
| Antipodal distance | 10 800 NM = 20 000 km | §8 |
| Test | Case | Method |
|---|---|---|
| Same longitude, both same hemi | Case 1 | Ch.lat → NM |
| Same longitude, different hemi | Case 2 | Sum lats → NM |
| Lons add to 180°, same hemi | Case 3 | 180° − sum of lats → NM |
| Lons add to 180°, diff hemi | Case 4 | Draw diagram, route via nearer Pole |
| Both at Equator (lat = 0) | Case 5 | Ch.long (shorter arc) → NM |
| Equal lats N & S, lons add to 180° | Case 6 | Always 10 800 NM |
| Hemisphere + Direction | GC Track Angle |
|---|---|
| North + East (→) | Increasing |
| North + West (←) | Decreasing |
| South + East (→) | Decreasing |
| South + West (←) | Increasing |
GC always changes direction towards the Equator. Mnemonic: DIID read from North-West clockwise.
| Q | Answer(s) |
|---|---|
| 1 | a) 12°40'S b) 109°55'S c) 39°50'N d) 21°55' |
| 2 | 2 285 NM | 4 232 km |
| 3 | a) 49°55'W b) 05°40'W c) 28°50'E d) 56°42'W |
| 4 | a) 01°29'N 002°05'W b) 03°36'S 001°13'E c) 00°26'N 005°22'E d) 67°24'N 004°44'E e) 00°01'N 014°36'E |
| 5 | a) 90/167 b) 482/893 c) 3 360/6 223 d) 660/1 222 e) 10 800/20 000 |
| 6 | a) 360°(T) b) No c) Over N Pole, then track reverses to 180°T |
| 7 | 70°40'N 023°00'W |
| 8 | 10°00'N 160°09'W |
| 9 | a) Nearer Equator (S of GC) b) Nearer Equator (N of GC) |
| 10 | c |
| 11 | c |