Water Vapor Pressure Equation:
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Water vapor pressure is the partial pressure of water vapor in any gas mixture. It represents the pressure exerted by water vapor molecules in the air and is a key parameter in meteorology, HVAC systems, and various industrial processes.
The calculator uses the water vapor pressure equation:
Where:
Explanation: This equation calculates the saturation vapor pressure of water at a given temperature, representing the maximum amount of water vapor the air can hold at that temperature.
Details: Accurate water vapor pressure calculation is essential for weather forecasting, humidity control, industrial processes, and understanding atmospheric phenomena like dew point and relative humidity.
Tips: Enter temperature in degrees Celsius. The calculator will compute the saturation vapor pressure in hectopascals (hPa).
Q1: What is the relationship between vapor pressure and temperature?
A: Vapor pressure increases exponentially with temperature. Warmer air can hold significantly more water vapor than cooler air.
Q2: How is vapor pressure related to relative humidity?
A: Relative humidity = (actual vapor pressure / saturation vapor pressure) × 100%. It indicates how close the air is to being saturated.
Q3: What are typical vapor pressure values?
A: At 20°C, saturation vapor pressure is about 23.4 hPa. Values range from about 6 hPa at 0°C to over 100 hPa at 50°C.
Q4: Why is vapor pressure important in meteorology?
A: It's crucial for predicting precipitation, fog formation, and understanding heat index and apparent temperature.
Q5: How does altitude affect vapor pressure?
A: While the saturation vapor pressure depends only on temperature, actual vapor pressure decreases with altitude due to lower atmospheric pressure.