Timescales and Structures in Vertical Transport in the Atmospheric Boundary Layer
25 November 2009 | 15:30
location: Room G , Faculty Applied Sciences
by Jerome Schalkwijk location: Room G , Faculty Applied Sciences
Vertical transport in the atmospheric boundary layer is commonly measured with the help of Eddy Covariance techniques, e.g. based on time averages measured at a single location.
This article is only available in Dutch.
