CAA NZ ATPL Theory - Flight Navigation General study materials
CAA NZ ATPL Theory - Flight Navigation General study resources

CAA NZ ATPL Theory - Flight Navigation General: Long-Range and Oceanic Navigation

CAA NZ ATPL Theory - Flight Navigation General · Work through your exam, one topic at a time.

All guide sections

Long-Range and Oceanic Navigation

Great circles and charts

A great circle is the shortest path between two points; its initial and final tracks differ, and the highest latitude reached is the vertex. A rhumb line has constant track but is longer. On a Mercator chart a great circle plots as a curve, so ocean tracks are drawn as straight lines between waypoints with the tracks re-measured at each one; the gnomonic chart shows great circles as straight lines.

Oceanic operation

  • Oceanic airspace uses prescribed tracks, normally with 50 nm or 100 nm lateral separation depending on the region and the RNP specification (RNP 10 or RNP 4 in the Pacific, RNP 4 in the North Atlantic).
  • Clearance fixes the route, level and Mach; position reports or ADS-C and CPDLC satisfy the reporting requirement.
  • Strategic Lateral Offset Procedure (SLOP) offsets the aircraft to the right of track, reducing the risk from an opposite-direction traffic error.
  • Contingency: if a weather deviation is needed, offset, advise ATC and return to track when able; loss of RNP capability requires informing ATC.
  • Equal time point and point of no return calculations use groundspeed, not TAS, in each direction.

Worked example

A and B are 1000 nm apart. Outbound groundspeed is 400 kt, return 500 kt. ETP distance from A = 1000 x 500 / (400 + 500) = 556 nm, reached after 556/400 = 1.39 h, about 1 h 23 min from A. Beyond that point the return takes longer than continuing.

Traps

Using TAS instead of groundspeed in ETP or PNR; assuming the return wind equals the outbound; applying the wrong RNP value to the airspace; and forgetting that a track offset must be reported and re-established correctly.