Biblio
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CoCoNet: Towards Coast to Coast Networks of Marine Protected Areas (from the shore to the high and deep sea), coupled with Sea-Based Wind Energy Potential. SCIRES-IT SCIentific RESearch and Information Technology 6, (2017).
CoCoNet: Towards Coast to Coast Networks of Marine Protected Areas (from the shore to the high and deep sea), coupled with Sea-Based Wind Energy Potential. SCIRES-IT : SCIentific RESearch and Information Technology 6, (2016).
Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth. Nature Communications 7, (2016).
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).
Climate change impacts on wind energy potential in the European domain with a focus on the Black Sea. Renewable & Sustainable Energy Reviews 81, (2017).
Diurnal asymmetry to the observed global warming. International Journal of Climatology (2015).
The Arctic Surface Climate in CMIP6: Status and Developments since CMIP5. Journal of Climate 33, (2020).
The Climatology of the Atmospheric Boundary Layer in Contemporary Global Climate Models. Journal of Climate 31, (2018).
Global climate models' bias in surface temperature trends and variability. Environmental Research Letters 9, (2014).
Surface air temperature changes in the high-latitude boundary layer. Report Series in Aerosol Science 180, (2016).
Surface air temperature variability in global climate models. Atmospheric Science Letters 15, (2014). Abstract
Trends in the normalized difference vegetation index (NDVI) associated with urban development of Northern West Siberia. Atmospheric Chemistry and Physics 16, (2016).
Complementary explanation of temperature response in the lower atmosphere. Environmental Research Letters 7, (2012).
Structuring of turbulence and its impact on basic features of Ekman boundary layers. Nonlinear processes in geophysics 20, (2013).
The climate role of shallow stably stratified atmospheric boundary layers. Proceedings of the 1st Pan-Eurasian Experiment (PEEX) Conference and the 5th PEEX Meeting. Report Series in Aerosol Science No. 163 (2015) (2015).
Stably stratified planetary boundary layer effects in northern hemisphere climate. Fundamentalnaya i prikladnaya gidrofizika 9, (2016).
Micro-climate on MEGA-computers. META (2012).
Marginal Ice Zone and Ice-Air-Ocean Interactions. Sea Ice in the Arctic, Past, Present and Future (2020).doi:10.1007/978-3-030-21301-5_3
Eurasian Winter Cooling: Intercomparison of Reanalyses and CMIP5 Data Sets. Atmospheric and Oceanic Science Letters 6, (2013).
Eurasian Cooling Patterns in the CMIP5 Climate Models. Izvestiya, Atmospheric and Oceanic Physics (2019).
Making better sense of the mosaic of environmental measurement networks: a system-of-systems approach and quantitative assessment. Geoscientific Instrumentation, Methods and Data Systems 6, (2017).
