Ionograms for six arctic stations have been scaled and analyzed. The diurnal variation of frequency spreading, range spreading, spread‐F type, spread‐F index, foF2, and fxF2 have been determined. Over the Canadian Archipelago spread F occurs throughout the 24‐hour period on a magnetically quiet day, even though the F region is illuminated. Differences are found between day and night. The diurnal variation of the severity of spread F can best be followed by means of the type of spread F and its index.