Climate is the statistics of weather, usually over a 30-year interval. It is measured by assessing the patterns of variation in temperature, humidity, atmospheric pressure, wind, precipitation, atmospheric particle count and other meteorological variables in a given region over long periods of time.
Once you have the saturation vapor pressure and the actual vapor pressure, relative humidity can be computed by dividing the actual vapor pressure by the saturation vapor pressure and then multiplying by 100 to convert the quantity to a percent. (7) Relative Humidity(RH) in percent =(E/Es)*100.
Definition of RELATIVE HUMIDITY: The ratio of vapour pressure in a sample of moist air to the saturation vapour pressure with respect to water at the same temperature, SPECIFIC HUMIDITY. HUMIDITY MIXING RATIO. SATURATED HUMIDITY MIXING RATIO. VIRTUAL TEMPERATURE. VAPOUR PRESSURE. SATURATION VAPOUR PRESSURE. RELATIVE HUMIDITY, EQUILIBRIUM STILL.