The footprint of a turbulent flux measurement defines its spatial context. With the onset of
long-term flux measurement sites over forests and other inherently inhomogeneous areas …

3.1 Eddy diffusivity and the gradient-transfer approach 101 3.2 Solutions of the equations of
diffusion 108 3.3 Similarity theory applied to diffusion 116 3.4 Statistical theory of dispersion …

Twenty years have passed since the first German-language edition of this book was
published. Subsequently, parallel German-and English-language editions were produced in …

This completely updated and revised Second Edition of the popular Workbook of
Atmospheric Dispersion Estimates provides an important foundation for understanding …

The flux footprint is the contribution, per unit emission, of each element of a surface area
source to the vertical scalar flux measured at height zm; it is equal to the vertical flux from a …

This paper gives the outline of a" meteorological preprocessor" for air pollution modeling. It
is shown how significantly more information can be extracted from routinely available …

A method for calculating the dispersion of plumes in the atmospheric boundary layer is
presented. The method is easy to use on a routine basis. The inputs to the method are …

Over the last 100 years, boundary layer meteorology grew from the subject of mostly near-
surface observations to a field encompassing diverse atmospheric boundary layers (ABLs) …

The characteristics of turbulence in the surface layer are well understood over spatially
homogeneous and smooth surfaces. Current theoretical knowledge is based on …

Air‐sea interaction data from a situation with pronounced unidirectional swell have been
analyzed. Measurements of turbulence at three levels (10, 18, and 26 m above mean sea …