Explanation:
Smog in Los Angeles is caused by temperature inversions (due to coastal mountains), which trap emissions, and photochemical reactions from sunlight, creating photochemical smog.
Explanation:
The saturated adiabatic lapse rate (about 0.6°C per 100m) is less than the dry adiabatic lapse rate (about 1°C per 100m). This is because when air is saturated, condensation releases latent heat, which partially offsets the cooling.
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