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Radiative cooling over flat and complex terrain: a forgotten term?
The atmospheric boundary layer undergoes a clear diurnal cycle. During daytime solar radiation heats the surface, and the warm land surface triggers thermals to develop, i.e. a convective boundary layer is created. During the day ...
Supervisor: Gert-Jan Steeneveld (Gert-Jan.Steeneveld@wur.nl)
Department: Meteorology and Air Quality Group |
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Turbulent dispersion under stable conditions
The ultimate goal would be to study turbulent dispersion in transitional stable boundary layer, including the night-to-day transition (e.g. according to the third GABLS intercomparison case (see www.atmo.ttu.edu/basu/GABLS3/).
T ...
Supervisor: Arnold Moene
Department: Meteorology and Air Quality Group |
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Scintillation Technique to estimate heat, water-vapour and momentum
Scintillation is the effect of trembling air above a hot road
caused by refraction (bending) of light as it interacts with turbulent eddies that transport heat and water vapor.
Scintillometers are instruments consisting of a tra ...
Supervisor: dr. ir. Oscar Hartogensis
Department: Meteorology and Air Quality Group |
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