Validation of GPS-based estimates of integrated water vapour for the Australian region and identification of diurnal variability
نویسندگان
چکیده
Accurate representation of the spatial and temporal distribution of water vapour in the atmosphere represents a significant challenge in current meteorological practice. The quality of quantitative precipitation forecasting and of model representation of hydrologic processes is clearly dependent on accurate initialisation of the atmospheric moisture distribution. Atmospheric water vapour is often quantified in kg/m2 as the vertically integrated mass of water vapour per unit area, or in mm as the height of an Aust. Met. Mag. 55 (2006) 131-148
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