Curriculum Vitae, Alastair D. Jenkins

Based on our three rather different velocity profiles — an exponential profile modelling a near-surface shear layer, a profile varying as z 1/7 modelling a turbulent bottom

It is the long-averaged surface flux fitted to a Gaussian profile which is normally applied as a boundary condition in atmospheric dispersion modelling. This practice

Fourth report of the Photochemical Exchange of ozone between the atmospheric boundary layer and the free Near-infrared spectroscopy and spectral mapping of

From south to north, the Pyrenees consists of the Ebro foreland basin; the South Pyrenean Unit, a fold-and-thrust belt consisting of Mesozoic and Cenozoic sedimentary successions;

Outside of the surface viscous layer and the bottom boundary layer the turbulent flux is not related to the wave-induced shear so that eddy viscosity parameterizations cannot

For a given internal wave energy at depth, an increase in near-surface stratification will result in greater internal wave horizontal velocity approaching the surface and

In the marine boundary layer, atmospheric pressure adjustments to sharp sea surface temperature gradients lead to surface wind convergence, which anchors a narrow band of

With these measurements, we have also been able to verify in different areas of study, that the Land Surface Temperature during the night does not depend on the turbulence, but