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This analysis explores the relationship between temperature and water vapor content in the air, specifically at sea level pressure (760 torr) under various relative humidity (R.H.) conditions. The study examines how varying relative humidity—ranging from 0% to 100%—affects the percentage of water vapor content in the air, providing critical insights into atmospheric science and meteorology as temperatures fluctuate from -10°C to +40°C.
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12 10 8 6 4 2 0 100% R.H. 50% R.H. Water vapor content of air (% of total volume) at sea level pressure (760 torr) 25% R.H. -10 0 10 20 30 40 50 Temperature (° C)