Biblio
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes. Boundary-layer Meteorology 125, 167-191 (2007). Abstract
Download: fulltext-9.pdf (680.31 KB)
Atmospheric planetary boundary layer feedback in climate system and triggering of climate change at high latitudes. EGU General Assembly 11, (2009).
The effect of stratification on the surface resistance for very rough vegetated and urban surfaces. Sixth International Conference on Urban Climate 415-418 (2006).
Diagnostic and prognostic equations for the depth of the stably stratified Ekman boundary layer. Quarterly J. Royal Meteorol. Soc. 25-46 (2002).
Similarity theory and calculation of the surface turbulent fluxes in stably-stratified atmospheric boundary layers. Atmospheric Boundary layers. Nature, theory and applications to moeling and environmental safety (2012).doi:10.1007/978-0-387-74321-9_4
Physic and parameterization of atmospheric stable boundary layers (invited lecture). ICTP Fall Colloquium on the Physics of Weather and Climate: Regional Weather Predictability and Modelling, Trieste, Italy, 29 September 10 October 2008. Abstract: the Colloquium web site (2008).
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).
The Height of the Atmospheric Planetary Boundary layer: State of the Art and New Development. National Security and Human Health Implications of Climate Change (2012).doi:10.1007/978-94-007-2430-3_13
Further comments on the equilibrium height of neutral and stable planetary boundary layers. Quarterly J. Royal Meteorol. Soc. 133, 265-271 (2007).
Modeling stable boundary layers (key lecture). SABLE Workshop. Abstracts and Presentations, November 12 - 16, 2006 (2006).
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
Arctic Clouds and Surface Radiation – a critical comparison of satellite retrievals and the ERA-Interim reanalysis. Atmospheric Chemistry and Physics (ACP) 12, (2012).
Uncertainties in Arctic sea ice thickness and volume: new estimates and implications for trends. The Cryosphere 8, (2014).
A model of solar coronal heating by classical inverse bremsstrahlung and generation of the solar wind. Astrophysical Journal 412, (1993).
Finite element modeling of ultrasound measurement systems for gas. Comparison with experiments in air. Journal of the Acoustical Society of America 144, (2018). Abstract
