Mixing Ratio Formula:
From: | To: |
The mixing ratio (MR) is defined as the mass of water vapor per unit mass of dry air. It's a fundamental measurement in atmospheric science for quantifying moisture content in air.
The calculator uses the mixing ratio formula:
Where:
Explanation: The formula calculates how much water vapor is present compared to dry air, expressed as grams of vapor per kilogram of dry air.
Details: Mixing ratio is crucial in meteorology for understanding atmospheric processes, cloud formation, and weather forecasting. It remains constant with changes in temperature and pressure.
Tips: Enter the mass of water vapor in grams and mass of dry air in kilograms. Both values must be positive numbers.
Q1: How is mixing ratio different from specific humidity?
A: While similar, mixing ratio uses mass of dry air as denominator, while specific humidity uses total air mass (dry air + vapor).
Q2: What are typical mixing ratio values?
A: In Earth's atmosphere, values range from near 0 g/kg in polar regions to 20 g/kg in tropical regions.
Q3: Why use grams per kilogram as units?
A: This unit convention makes the typically small values easier to work with and compare.
Q4: Does mixing ratio change with altitude?
A: The mixing ratio of an air parcel remains constant unless vapor is added/removed, even as it rises or descends.
Q5: How is this used in weather forecasting?
A: Mixing ratio helps predict dew point, cloud base height, and potential for precipitation.