On a dark and cloudy day, what is the predicted pattern for nitrogen dioxide and ground-level ozone readings?

Prepare for the AP Environmental Science (APES) test on Atmospheric Pollution. Use flashcards and multiple choice questions with detailed explanations to enhance your understanding of key concepts. Perfect your test readiness now!

Multiple Choice

On a dark and cloudy day, what is the predicted pattern for nitrogen dioxide and ground-level ozone readings?

Explanation:
On a dark, cloudy day, the amount of sunlight is minimal, which slows the photochemical reactions that produce ground-level ozone. Ozone at the surface forms when NO2 is broken apart by photons to produce atomic oxygen, which then combines with O2 to make O3. Without enough light, this step happens less, so ozone formation drops. At the same time, nitrogen dioxide can accumulate because its destruction by photolysis is reduced and ongoing emissions keep adding NO2 to the air. Additionally, any ozone that is present can be consumed by reactions with NO to form more NO2, reinforcing the drop in ozone. So nitrogen dioxide tends to increase while ground-level ozone decreases.

On a dark, cloudy day, the amount of sunlight is minimal, which slows the photochemical reactions that produce ground-level ozone. Ozone at the surface forms when NO2 is broken apart by photons to produce atomic oxygen, which then combines with O2 to make O3. Without enough light, this step happens less, so ozone formation drops. At the same time, nitrogen dioxide can accumulate because its destruction by photolysis is reduced and ongoing emissions keep adding NO2 to the air. Additionally, any ozone that is present can be consumed by reactions with NO to form more NO2, reinforcing the drop in ozone. So nitrogen dioxide tends to increase while ground-level ozone decreases.

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