Why it matters at the radio
It helps estimate whether high-angle paths such as NVIS are possible. Oblique paths can use frequencies above the vertical critical frequency because they meet the layer at a shallower angle.
What to watch in the field
Use current foF2 or ionosonde data near the path, then confirm on air. Local data can change quickly and may not represent the entire route.
The common misunderstanding
Using critical frequency and MUF as interchangeable terms.
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