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The scattered light of solar radiance near the infrared ray area was observed to measure and absorption lines. The changes of and equivalent width were calculated on the basis of the measurement. equivalent width showed negative correlation with the amount of solar radiance; equivalent width had a tendency to diminish as the amount of the solar radiance increased and to increase as the amount of the solar radiance decreased. On the other hand, equivalent width showed the positive correlation with the amount of solar radiance. Especially it was noted that the sum of equivalent width of absorption lines created by and in a day was fairly constant. It is implied that the constant equivalent width is caused by the complementary development of photodissociation and recombination in and .

Diurnal Variation of Equivalent Width of H2O and O2in Earth's Atmosphere