When the moisture in the air that is in contact with the earth is
condensed above the freezing point, dew is formed. When below the
freezing point, frost is formed or deposited on the earth. It is readily
understood from this that the surface on which the frost is deposited is
at a freezing temperature, while the air above it may not be freezing.
Naturally, you can expect frost when the temperature falls to a point 8°
or 10° above the freezing point. Clear, calm nights are favorable for
frost, because the absence of clouds helps radiation, that is, it draws
heat away from the earth. If there are clouds, it prevents this
radiation.