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This article delves into the concepts of specific humidity and relative humidity, two key terms essential for understanding atmospheric moisture. Specific humidity measures the mass of water vapor in a given mass of air, while relative humidity compares the current water vapor in the air to the maximum it can hold at a given temperature. We explore their differences, applications in meteorology, and implications for weather forecasting and climate studies, providing readers with a clearer comprehension of these fundamental concepts.
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Two key terms with which to begin: • Specific humidity; • Relative humidity.
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