https:\/\/climate.ncsu.edu\/edu\/Heat<\/a><\/p>\n\n\n\n https:\/\/www.earthonlinemedia.com\/ebooks\/tpe_3e\/atmospheric_moisture\/phase_changes.html<\/a><\/p>\n\n\n\n Mixing Ratio (r): <\/strong>The\nactual amount of water vapor in an air parcel (Mass of water vapor per unit\nmass of dry air – grams of water\/ kg of air) [g\/kg]<\/p>\n\n\n\n Saturation Mixing\nRatio (rs): <\/strong>The amount of water vapor in saturated air at a specific\ntemperature [g\/kg]<\/p>\n\n\n\n Relative Humidity (RH):<\/strong> The RATIO of the amount\nof water actually in the air compared to the max. amount of water vapor\nrequired for saturation at that particular temperature and pressure [%]<\/p>\n\n\n\n RH = 100% x\n( r \/ rs)<\/strong><\/p>\n\n\n\n <\/p>\n\n\n\n <\/p>\n\n\n\n <\/p>\n","protected":false},"excerpt":{"rendered":" Introduction to water phase change and importance in meteorology https:\/\/climate.ncsu.edu\/edu\/Heat https:\/\/www.earthonlinemedia.com\/ebooks\/tpe_3e\/atmospheric_moisture\/phase_changes.html Moisture in the atmosphere Mixing Ratio (r): The actual amount of water vapor in an air parcel (Mass of water vapor per unit mass of dry air – grams of water\/ kg of air) [g\/kg] Saturation Mixing Ratio (rs): The amount of water vapor … Continue reading Moisture<\/span> Moisture in the atmosphere<\/h2>\n\n\n\n