Biblio
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Numerical experiments with assimilation of the mean and unresolved meteorological conditions into large-eddy simulation model. MEGAPOLI "Emissions, urban, regional and Global Atmospheric POLlution and climate effects, and Integrated tools for assessment and mitigation" project (2010).at <http://arxiv.org/abs/1002.1632> Abstract
Download: Numerical experiments with assimilation of the mean and unresolved meteorological conditions into large-eddy simulation model.pdf (421.03 KB)
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)
Large-eddy simulation of PBLs. (2007).
Simulation of Ekman boundary layers by large eddy model with dynamic mixed subfilter closure. Journal of Environmental Fluid Mechanics 4, 273-303 (2004). Abstract
Download: fulltext-16.pdf (498.33 KB)
Methods and Measurement Tools in PBL: On combination of artificial neural network and hydro-dynamic turbulence-resolving modelling for turbulent flows in urban environment. article published in ENEA special report issue on "ATMOSFERA" (2007).
Structuring of turbulence and its impact on basic features of Ekman boundary layers. Nonlinear processes in geophysics 20, (2013).
Trends in the normalized difference vegetation index (NDVI) associated with urban development of Northern West Siberia. Atmospheric Chemistry and Physics (ACP) 16, (2016).
Large-scale urban boundary layer turbulence: An example of large-eddy simulations for a megacity. ENVIROMIS-2010 (2010). Download: Esau_2010_ENVIROMIS2010.doc (22.5 KB)
Spatial structure and temporal variability of a surface urban heat island in cold continental climate. Theoretical and Applied Climatology 137, (2019). Abstract
Convective feedback in climate change. International Conference on Computational Information Technologies for Environmental Sciences: CITES-2007, 20-25 July, Tomsk, Russia (The reviewed paper is to appear in "Russian Computational Technology") (2007).
Complementary explanation of temperature response in the lower atmosphere. Environmental Research Letters 7, (2012).
Non-dimensional governing parameters of turbulent planetary boundary layers. Bjerknes Centannualy Conference (2004).
First results from coupled atmosphere-ocean large-eddy simulations. EGU General Assembly, 13-18 April, Vienna, Austria, /Geophysical Research Abstracts/, *10*, EGU2008-A-01784 (2008).
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
Warmer urban climates for development of green spaces in northern Siberian cities. Geography, Environment, Sustainability 4, (2016).
Variability of temperature and cloudiness in the Arctic planetary boundary layer. International Polar Year Science Conference (2010).
Exogenous drivers of surface urban heat islands in Northern West Siberia. Geography, Environment, Sustainability 11, (2018). Abstract
Warmer Climate of Arctic Cities. The Arctic: Current Issues and Challenges (2020).at <https://novapublishers.com/shop/the-arctic-current-issues-and-challenges/>
Intercomparisons of turbulence statistics derived from large-eddy simulation and field databases. General EGU assembly, 15-20 April, Vienna, Austria, Geophysical Research Abstracts, 9, 01064 (2007).
Contrasting Vertical Structure of Recent Arctic Warming in Different Data Sets. Atmospheric and Climate Sciences 3, (2013).
Vi kan skaffe mer kunnskap om giftlokket. Bergens Tidende (2011). Download: BT-070111-Esau-Luftkvalitet.pdf (1.4 MB)
