Biblio
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Energetics of turbulence, Ri-critical, and a new closure model for stable stratification. Atmospheric boundary layer flows in air pollution modelling , VKI LS 2008-06 (ed. by J.P.A. van Beek, J.-M. Buchlin, A. Petrosyan), von Karman Institute for Fluid Dynamics, ISBN-13 978-2-930389-85-0, D/208/0238/526, 3.1-3.7 (2008).
Calculation of the height of stable boundary layers in practical applications. Boundary-layer Meteorology 389-409 (2002).at <http://www.springerlink.com/content/100245/?p=43e84a3972f3443fbe3e13aeb2578da0&pi=0>
Further comments on the equilibrium height of neutral and stable planetary boundary layers. Quarterly J. Royal Meteorol. Soc. 133, 265-271 (2007).
On the exploitation of polarimetric ratio for oil spill detection. Electronic proceedings (EUSAR) 2016:7559371, (2016).
Long-term variation in TOMS ozone over 60 deg.-70 deg. S. Geophysical Research Letters 24, 2295-2298 (1997).
Total ozone variation between 50 and 60 N. Geophysical Research Letters 32, (2005). Download: 2005GL024012.pdf (225.86 KB)
Adaptively varying-coefficient spatiotemporal models. Journal of the Royal Statistical Society: Series B (Statistical Methodology) 71, (2009). Abstract
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