Biblio
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Climatology of the Arctic planetary boundary layer. Atmospheric Turbulence: Prediction, Measurement, and Effects 3-58 (2010).at <https://www.novapublishers.com/catalog/product_info.php?products_id=9521>
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)
Physical mechanism and quantitative assessment of the planetary boundary layer feedback in the climate system. The IARU International Scientific Congress on Climate Change (2009).
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)
Planetary Boundary Layer Feedback and Its Role in Climate Change. 16B.3, /18th Symposium on Boundary Layers and Turbulence/, American Geophysical Society, 9-13 June, Stockholm, Sweden (2008).
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).
Vertical structure of the Arctic warming: The effect of the Arctic planetary boundary layer decoupling. Arctic Science Summit Week (2009).
Non-local effects of large eddies in surface layer. Computational Technology (Russian) 9, 71-85 (2004).
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)
Convective cloud fields in the Atlantic sector of the Arctic: Satellite and ground-based oservations. Izvestiya, Atmospheric and Oceanic Physics 51, (2015). Download: esau_chernokulsky_2014_convective_cloud_fields_in_the_atlantic_sector_of_the_arctic.pdf (2.74 MB)
Non-Linear Response of Turbulent Fluxes on Openings in Ice Cover of the Arctic Ocean. The First CliC International Science Conference (2005).
The planetary boundary layer feedbacks in polar latitudes. World Climate Research Programme workshop on seasonal to multi-decadal predictability of polar climate (2010).at <http://www.atmosp.physics.utoronto.ca/SPARC/PolarWorkshop/main.html>
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)
Systematic errors in northern Eurasian short-term weather forecasts induced by atmospheric boundary layer thickness. Environmental Research Letters 13:125009, (2018). Abstract
Turbulence-resolving simulations of circulations near ice edge. General EGU assembly, 15-20 April, Vienna, Austria, Geophysical Research Abstracts, 9, 01318 (2007).
Turbulent Prandtl Number in Stably Stratified Atmospheric Boundary Layer: Intercomparison between LES and SHEBA Data. http://ejournal.windeng.net 1-17 (2007).
Structuring of turbulence and its impact on basic features of Ekman boundary layers. Nonlinear processes in geophysics 20, (2013).
Large-eddy simulation of PBLs. (2007).
Numerical Experiments for Central Paris with Urbanized Large-Eddy Simulation Model PALM (MEGAPOLI Del 2.4). MEGAPOLI Newsletters (2010). Abstract
Download: MEGAPOLI_NewsLet07.pdf (8.15 MB)
Large-eddy simulations of geophysical turbulent flows with applications to planetary boundary layer research. Proceedings of 5th conference on computational mechanics "MekIT'09", Trondheim, 26-27 May 7-37 (2009).
Formulation of the planetary boundary layer feedback in the Earth´s climate system. Computational Technologies 13, 95-103 (2008). Abstract
Download: Esau_2008_Computational_Technologies_v13n3pp90_103_Formulation_PBL_feedback_scanned.pdf (2.74 MB)
Complementary explanation of temperature response in the lower atmosphere. Environmental Research Letters 7, (2012).
