This page is part of the N0NJY General Class self-study course for Technician operators upgrading to General.
Understanding propagation separates a skilled HF operator from someone who simply turns the radio on and hopes for the best. HF signals travel worldwide because they interact with the ionosphere — a region of the upper atmosphere that can refract radio waves back to Earth. The solar cycle controls the ionosphere, so learning to read solar conditions is a core HF skill.
The ionosphere extends from roughly 60 km to 1,000 km altitude. Solar radiation ionizes gas molecules, creating free electrons that can refract radio waves. It is divided into layers:
D Layer (60–90 km)
Exists only during daylight. The D layer absorbs lower HF frequencies rather than refracting them.
This is why 160, 80, and 40 meters are largely useless for long-distance contacts during the day. The D layer
disappears at night, allowing those signals to reach the F layer and propagate long distances.
E Layer (90–150 km)
Forms during daylight, mostly disappears at night. Can support propagation at 1,000–2,000 km distances.
Sporadic-E (Es) is unpredictable dense ionization in the E layer that can enable propagation
on frequencies up to 150 MHz. Sporadic-E is common in late spring and early summer.
F Layer (150–500 km)
The primary layer for long-distance HF propagation. Splits into F1 and F2 during the day; merges at night.
The F2 layer can support globe-spanning propagation. It persists at night because ion recombination is slow
at high altitudes.
Solar activity follows an approximately 11-year cycle. More solar activity means better ionospheric ionization and better propagation on the higher HF bands.
When a signal is launched at a low angle, it travels up to the ionosphere and is refracted back to Earth at some distance away. The area between the transmitter and the nearest return point is the skip zone — unreachable by either ground wave or sky wave.
Maximum Usable Frequency (MUF): The highest frequency that will be refracted by the ionosphere for a given path at a given time. Above the MUF, signals pass through and are lost to space. Operating near but below the MUF gives the best signals.
Lowest Usable Frequency (LUF): The lowest frequency usable for a given path. Below the LUF, D-layer absorption is too high for the signal to survive the trip.
Near Vertical Incidence Skywave (NVIS) is designed specifically for short-range HF communication — typically 0 to 300 miles. Instead of low-angle radiation, NVIS uses nearly vertical radiation angles. The signal goes almost straight up, hits the F layer, and falls almost straight back down, eliminating the skip zone.
Transequatorial Propagation (TEP): Signals cross the geomagnetic equator. Primarily affects 6 meters, most common in spring and fall. Can enable contacts exceeding 10,000 miles on 6 meters.
Sporadic-E: Unpredictable E-layer enhancement enabling VHF propagation to hundreds or thousands of miles. Common on 6 meters and 10 meters during late spring and summer.
Meteor Scatter: Signals reflect off ionized meteor trails. Brief bursts (milliseconds to seconds) on VHF/UHF. Requires high-speed digital modes.
Tropospheric Ducting: Temperature inversions in the lower atmosphere create a refractive duct for VHF/UHF signals. Distances of hundreds to thousands of miles are possible. Common over water and in coastal areas — relevant to your location at Caswell Beach.
Q1 (G3A01) — Which are good indicators of approaching solar maximum?
Q2 (G3B07) — What is NVIS propagation?
Q3 (G3C01) — Which frequency range is most useful for NVIS propagation?
Q4 (G3A04) — What does a high K-index indicate?
Q5 (G3B05) — What is the maximum usable frequency (MUF)?
Q6 (G3C05) — Which propagation type most likely allows 6-meter communication between stations 10,000 miles apart?
Q7 (G3A12) — What is the effect of a sudden ionospheric disturbance on HF propagation?
Q8 (G3B03) — Why is the F2 region mainly responsible for the longest long-distance propagation?