Biblio
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes. Atmospheric Boundary Layers: Nature, Theory and Applications to Environmental Modelling and Security 11-35 (2007).doi:10.1007/978-0-387-74321-9_3 Abstract
Download: fulltext-8.pdf (727.04 KB)
Modeling stable boundary layers (key lecture). SABLE Workshop. Abstracts and Presentations, November 12 - 16, 2006 (2006).
The effect of baroclinicity on the depth of neutral and stable planetary boundary layers. Quart, J. Roy. Met. Soc. 3339-3356 (2003).
On integral measures of the neutral, barotropic planetary boundary layers. Boundary-layer Meteorology 371-379 (2002).at <http://www.springerlink.com/content/100245/?p=43e84a3972f3443fbe3e13aeb2578da0&pi=0>
What do we need from experiments to better model physical processes in stable boundary layers?. CD-ROM Sodankylä Seminar on Stable Boundary Layers. Sodankylä, Finland, 30-31 August 2004, Finnish Meteorological Institute. (2004).
A sight on air pollution in industrial districts (invited lecture). International Meeting: Biferno Valley: Atmosphere and Fluvial Environment (Regione Molise / ENEA), Termoli, Italy, 7.10.2008. Abstract: the Meeting proceedings (2008).
Similarity theory and calculation of turbulent fluxes at the surface for the stably stratified atmospheric boundary layers. 7th Annual EMS Meeting, 1-5 October, San Lorenzo de El Escorial, Spain, EMS7/ECAM8 Abstracts, 4 (2007).
Near-surface turbulent fluxes in stable stratification: calculation techniques for use in general circulation models. Quart. J. Roy. Met. Soc. 1571-1587 (2002).
Monitoring and forecasting of personal environment. Fundamentalnaya i prikladnaya gidrofizika 9, (2016).
On the velocity gradient in the stably stratified sheared flows. Part 1: Asymptotic analysis and applications. Boundary-Layer Meteorology 135, (2010). Abstract
Download: On the Velocity Gradient in Stably Stratified Sheared Flows. Part 2- Observations and Models.pdf (349.05 KB)
On the exploitation of polarimetric ratio for oil spill detection. Electronic proceedings (EUSAR) 2016:7559371, (2016).
Total ozone variation between 50 and 60 N. Geophysical Research Letters 32, (2005). Download: 2005GL024012.pdf (225.86 KB)
Long-term variation in TOMS ozone over 60 deg.-70 deg. S. Geophysical Research Letters 24, 2295-2298 (1997).
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
