The diurnal variation of various meteorological parameters in the Planetary Boundary Layer at different altitudes has been studied through a remote sensing instrumentation and a sonic anemometer. RASS-SODAR integrated system allowed the definition of the vertical temperature profiles and the determination of the vertical wind speed and direction profiles. The Sonic Anemometer provided the dataset used to obtain the time trend of other meteorological and dispersive parameters, and to evaluate the PBL turbulence and heat exchange.
Planetary Boundary Layer: a model validation.
PECORARI, ELIANA;RAMPAZZO, Giancarlo
2011-01-01
Abstract
The diurnal variation of various meteorological parameters in the Planetary Boundary Layer at different altitudes has been studied through a remote sensing instrumentation and a sonic anemometer. RASS-SODAR integrated system allowed the definition of the vertical temperature profiles and the determination of the vertical wind speed and direction profiles. The Sonic Anemometer provided the dataset used to obtain the time trend of other meteorological and dispersive parameters, and to evaluate the PBL turbulence and heat exchange.
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