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vapour pressure deficit with the data of the previous example . The actual vapour pressure can also be calculated from the relative humidity. Depending on the availability of the humidity data, different equations should be used. Tdry-Twet wet bulb depression, with Tdry the dry bulb and Twet the wet bulb temperature [°C]. The average value of the atmospheric pressure is 81.8 kPa. Determine the atmospheric pressure and the psychrometric constant at an elevation of 1800 m. Values for atmospheric pressure as a function of altitude are given in Annex 2 (Table 2.1). Meteorological data can be expressed in several units. Conversion factors between various units and standard S. I. units are given in Annex 1. Climatic parameters, calculated by means of the equations presented in this chapter are tabulated and displayed for different meteorological conditions in Annex 2. Only the standardized relationships are presented in this chapter. The background of certain relationships and more information about certain procedures are given in Annex 3. Annexes 4, 5 and 6 list procedures for the statistical analysis, assessment, correction and The hottest product galaxy fox all over print air jordan 13 sneakerscompletion of partial or missing weather data. The methods for calculating evapotranspiration from meteorological data require various climatological and physical parameters. Some of the data are measured

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