Biblio
Filters: Author is Zilitinkevich, Sergej [Clear All Filters]
An enhanced integrated approach to knowledgeable high-resolution environmental quality assessment. Environmental Science and Policy 122, (2021).
Closure schemes for stably stratified atmospheric flows without turbulence cutoff. Journal of the Atmospheric Sciences 73, (2016).
Monitoring and forecasting of personal environment. Fundamentalnaya i prikladnaya gidrofizika 9, (2016).
Pan-Eurasian Experiment (PEEX): Towards a holistic understanding of the feedbacks and interactions in the land-Atmosphere-ocean-society continuum in the northern Eurasian region. Atmospheric Chemistry and Physics (ACP) 16, (2016).
Diurnal asymmetry to the observed global warming. International Journal of Climatology (2015).
Revisiting the turbulent prandtl number in an idealized atmospheric surface layer. Journal of the Atmospheric Sciences 72, (2015).
Atmospheric boundary layer over steep surface waves. Ocean Dynamics 64, (2014). Download: troitskaya_2014_atmospheric_boundary_layer_over_steep_surface_waves.pdf (2.67 MB)
Pan Eurasian Experiment (PEEX) - A research initiative meeting the grand challenges of the changing environment of the Northern Pan-Eurasian Arctic Boreal Areas. Geography, Environment, Sustainability (2014).doi:10.24057/2071-9388-2014-7-2-13-48 Download: lappalinen_esau_etal_2014_ges_peex_description.pdf (730.59 KB)
Analysis of remote sensing monitoring of the lower atmosphere temperature profile in Bergen, Norway. Russian Meteorology and Hydrology 38, (2013).
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
Links between observed micro-meteorological variability and land-use patterns in the highveld priority area of South Africa. Meteorology and atmospheric physics (Print) 118, (2012).
Links between observed micrometeorological variability and land-use patterns in the highveld priority area of South Africa. Meteorology and Atmospheric Physics 118, 16 (2012). Download: Esau_etal_2012_MAPh_V118N3-4pp129-142_doi10.1007_s00703-012-0218-4.pdf (993.75 KB)
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
On the velocity gradient in the stably stratified sheared flows. Part 2: Observations and models. 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 role of the planetary boundary layer depth in the climate system. Advances in Science and Research 4, (2010). Abstract
Download: On the role of the planetary boundary layer depth in the climate system.pdf (301.54 KB)
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)
Energy- and flux-budget turbulence closure model for stably stratified geophysical flows. 4th International Conference on Frontiers of Nonlinear Physics (2010). Download: Nizniy_Novgorod_2010.pdf (408.12 KB)
MEGAPOLI: concept of multi-scale modelling of megacity impact on air quality and climate. Advances in Science & Research 4, (2010). Abstract
Download: asr-4-115-2010.pdf (3.31 MB)
A Micro-Meteorological Experiment in the Atmospheric Boundary Layer in Highveld Region. International Conference on Planetary Boundary Layer and Climate Change 13, no. 012011, (2010). Download: 1755-1315_13_1_012011.pdf (905.73 KB)
Principal comments on numerical simulation of homogeneous stably stratified turbulence. Boundary-Layer Meteorology (2010).doi:10.1007/s10546-010-9484-1 Download: fulltext-32.pdf (99.83 KB)
Atmospheric planetary boundary layer feedback in climate system and triggering of climate change at high latitudes. EGU General Assembly 11, (2009).
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part II: The role of internal gravity waves. Boundary-Layer Meteorology (2009).doi:10.1007/s10546-009-9424-0
