Biblio
Filters: Author is Esau, Igor [Clear All Filters]
Air–sea interaction under low and moderate winds in the Black Sea coastal zone. Estonian Journal of Engineering 18, (2012).
Amplification of Turbulent Exchange due to Surface Thermal Heterogeneity: Study of Polar Ocean Leads. Stable Atmospheric Boundary Layer Workshop (2006).
Amplification of turbulent exchange over wide Arctic leads: Large-eddy simulation study. Journal of Geophysical Research (Atmospheres) 112, (2007). Download: 2006JD007225.pdf (966.61 KB)
Analysis of remote sensing monitoring of the lower atmosphere temperature profile in Bergen, Norway. Russian Meteorology and Hydrology 38, (2013).
The analysis of results of remote sensing monitoring of the temperature profile in lower atmosphere in Bergen (Norway). Russian Meteorology and Hydrology 38, (2013). Download: esau_etal_2013_the_analysis_of_results_of_remote_sensing_monitoring.pdf (338.68 KB)
Analysis of the vertical temperature structure in the Bergen valley, Norway, and its connection to pollution episodes, and its connection to pollution episodes. Journal of Geophysical Research (JGR): Atmospheres 119, (2014).
Anthropogenic and natural drivers of a strong winter urban heat island in a typical Arctic city. Atmospheric Chemistry and Physics (ACP) 18, (2018).
Anthropogenic heating strongly amplifies the urban heat island in Arctic cities. Atmospheric Chemistry and Physics (ACP) 18, (2018).
Application of a large-eddy simulation database to optimisation of first-order closures for neutral and stably stratified boundary layers. Atmospheric Boundary Layers: Nature, Theory and Applications to Environmental Modelling and Security 51-70 (2007).at <http://www.springerlink.com.pva.uib.no/content/978-0-387-74318-9/#section=167167&page=1&locus=11> Abstract
Download: fulltext-12.pdf (1.43 MB)
On Application of Artificial Neural Network Methods in Large-eddy Simulations with Unresolved Urban Surfaces. Modern Applied Science 4, (2010). Abstract
Download: On Application of Artificial Neural Network Methods in Large-eddy Simulations with Unresolved Urban Surfaces.pdf (836.47 KB)
Application of large-eddy simulation for optimization of the first-order turbulence closures for neutral and stably-stratified boundary layers. Atmospheric Boundary layers. Nature, theory and applications to moeling and environmental safety (2012).doi:10.1007/978-0-387-74321-9_5
Asymmetry of the surface air temperature response on climatologic heat imbalance due to differences in the planetary boundary layer height. Geophysical Research Abstracts 15, (2013).
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)
Atmospheric boundary layers in storms: advanced theory and modelling applications. Advances in Geosciences 47-49 (2005).
Atmospheric boundary layers in storms: advanced theory and modelling applications. The 6th Plinius International Conference on Mediterranean Storms (Genoa Naples Palermo Palma de Mallorca Barcelona Marseille Genoa), 17-24 October 2004. (2004).
Atmospheric planetary boundary layer feedback in climate system and triggering of climate change at high latitudes. EGU General Assembly 11, (2009).
Baroclinic Ekman Layer. Abstracts: 15th AMS Symposium on Boundary Layers and Turbulence, Wageningen, The Netherlands, 15-19 July 2002 (2002).
Bjerknes compensation and the multi-decadal variability of heat transports in the Arctic. Climatology of the high latitudes. Extended proceedings of the joint GCR and PEEX workshop at NERSC 29.09.2015 (2016).
Bjerknes compensation in the Bergen Climate Model. Climate Dynamics (2016).
Bjerknes compensation in the CMIP5 Climate Models. Journal of Climate (2018).doi:10.1175/JCLI-D-18-0058.1
