CHEM 1001 Study Guide - Midterm Guide: Sulfur Dioxide, Electromagnetic Radiation, Air Conditioning

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Spectroscopy: visible spectrometers measure the amount of light absorbed or transmitted, transmittance the % of light that passes through a sample, absorbance the amount of light absorbed by a sample. Ozone in the troposphere: surface level ozone, formed by smog, 0-10 miles. Ozone in the stratosphere: ozone layer, 10-31 miles, breaks down into o2 and o. Ozone layers protects us from harmful uv light because uv-a, uv-b, and uv-c light doesn"t pass through the ozone layer. Mechanisms for ozone formation and destruction: natural mechanisms = chapman cycle, anthropogenic mechanisms = catalytic destruction by free radicals, especially above antarctica by cl and br atoms in the antarctic spring. Polar stratospheric clouds (pscs): clouds in the winter polar stratosphere at altitudes of. 15,000-25,000: formation: winds circulate form a vortex that prevents warmer air from entering the region, reactions on pscs lead to ozone destruction, seasonal cycle of ozone destruction in antarctica: due to winter temps (june-

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