A model algorithm for defining the vertical profile of absolute humidity by ground measurements of humidity

In this study a double model algorithm is developed for the simulation of the vertical profiles of monthly values of absolute humidity. The thrust of the algorithm is that is depends on the use of ground measurements for humidity and is based upon the use of two model relations for altitudes above and below 1 Km respectively. Monthly absolute humidity profiles as estimated using the specially constructed double model algorithm compare well with those calculated with the use of radiosonde data for the time period 1980–1990 (Helliniko station, Southern Greece). In particular the model estimation is very satisfactory at altitudes above the Planetary Boundary Layer and rather satisfying at altitudes below 1 Km. This implies that the model algorithm may be useful in supporting climatological studies in areas where lack of relevant information on the vertical distribution of water vapour is recognised.