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BandPass Academy Amateur radio licence exam practice

Units published 20/31 Built 8 Oct 2026

G2 · Published 8 October 2026 ·

Angles, Paths and the Bands That Behave Differently

This unit takes the same physics further: what the angle of radiation does to where your signal lands, why a path sometimes runs the long way round the world, and why 160 metres and 6 metres are the two bands that ignore most of the rules.

  • Band 80 m
  • Study time 18
  • Level Stretch
  • questions 10
Waveform and antenna diagram for HF Propagation and Space Weather
HF Propagation and Space Weather — waveform overlay and radiation pattern

Pre-flight briefing

Angle of radiation decides the distance

For a given band and a given layer height, only a limited range of takeoff angles produces a return to earth. The highest angle that still returns a signal is the critical angle: transmit steeper than that and the wave passes straight through the layer into space. Shallow angles give long hops, steep angles give short hops, and the first skywave hop on 40 metres at a low angle may land 400 kilometres away while the same band fired nearly vertically covers 100 to 300 kilometres.

The number of hops determines the total distance. A single F2 hop reaches roughly 4,000 kilometres at a good angle, so a 12,000 kilometre contact is three hops, each with its own loss. That is why multi-hop paths are weaker than single-hop ones even when both ends have the same equipment, and why a path that looks geometrically possible may be unusable in practice.

Short path, long path and the terminator

Every two points on earth are connected by two great-circle routes: the short path, which is the direct way, and the long path, which goes the other way round, 180 degrees different in bearing. Long-path contacts happen when the short path is in daylight or in absorption while the long path is in darkness - typically around sunrise and sunset - and they are recognisable by a signal that arrives from the wrong direction with an echo or a hollow quality.

Two related effects are worth knowing. Signals crossing the geomagnetic equator can be enhanced by transequatorial propagation, a mode that produces surprisingly strong contacts between stations at roughly equal magnetic latitudes. And at the terminator itself, the grey line, absorption along one end of the path is low while the F layer is still illuminated, which is the classic window for 80 metre DX.

The two bands that misbehave

160 metres is difficult for reasons that are mostly not ionospheric. It suffers from high atmospheric and man-made noise because the band is narrow and close to the noise floor, it needs a physically large antenna for efficiency, and in summer the static from distant thunderstorms makes it nearly unusable at any distance. In winter, at night, with a well-designed vertical and a good radial field, it produces intercontinental contacts.

Six metres is the opposite puzzle: it is a VHF band that occasionally behaves like HF. Sporadic E opens it to a thousand kilometres or more with no warning; transequatorial propagation carries it between the Americas and southern Europe or Africa; aurora and meteor scatter support brief contacts at high latitudes. Most of the time it is empty, which is exactly why 6 metre operators spend so long listening.

Terms you must be able to define
TermWhat the examiner wants to hear
Critical angleThe steepest takeoff angle at which a signal at a given frequency is still returned by the layer.
HopOne trip from the antenna up to the ionosphere and back to earth.
Long pathThe great-circle route in the opposite direction from the short path, 180 degrees away in bearing.
Transequatorial propagationEnhanced propagation across the geomagnetic equator between stations at similar magnetic latitudes.
Sporadic EUnpredictable dense E-region ionisation that opens 6 metres over long distances.

Question deck 10 questions

G3B01 Core

What is the critical angle for an ionospheric layer at a given frequency?

G3B02 Core

Approximately how far can a single F2 layer hop carry a signal?

G3B03 Core

What is meant by a long-path contact?

G3B04 Core

Why is the 160 metre band often unusable in summer?

G3B05 Stretch

What is transequatorial propagation?

G3B06 Core

What does the eleven-year sunspot cycle affect for HF operators?

G3B07 Core

What is a propagation beacon used for?

G3B08 Stretch

Why do contacts on 6 metres often appear with no warning and last only minutes?

G3B09 Stretch

Why is ground-wave propagation significant on the low HF bands but not at VHF?

G3B10 Stretch

A signal arrives from a bearing roughly 180 degrees from the short path with a hollow, echo-like quality. What is happening?