Biblio
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Trends in the normalized difference vegetation index (NDVI) associated with urban development of Northern West Siberia. Atmospheric Chemistry and Physics 16, (2016).
Surface air temperature variability in global climate models. Atmospheric Science Letters 15, (2014). Abstract
Surface air temperature changes in the high-latitude boundary layer. Report Series in Aerosol Science 180, (2016).
Structuring of turbulence and its impact on basic features of Ekman boundary layers. Nonlinear processes in geophysics 20, (2013).
Stably stratified planetary boundary layer effects in northern hemisphere climate. Fundamentalnaya i prikladnaya gidrofizika 9, (2016).
Scientific challenges of convective-scale numerical weather prediction. Bulletin of The American Meteorological Society - (BAMS) (2018).doi:10.1175/BAMS-D-17-0125.1 Abstract
Reassessing changes in Diurnal Temperature Range: Intercomparison and evaluation of existing global dataset estimates. Journal of Geophysical Research (JGR): Atmospheres 121, (2016).
Reassessing changes in Diurnal Temperature Range: A new dataset and characterization of data biases. Journal of Geophysical Research (JGR): Atmospheres 121, (2016).
Reassessing changes in diurnal temperature range: A new data set and characterization of data biases. Journal of Geophysical Research (JGR): Atmospheres 121, (2016).
Micro-climate on MEGA-computers. META (2012).
Marginal Ice Zone and Ice-Air-Ocean Interactions. (2020).doi:10.1007/978-3-030-21301-5_3
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).
Global climate models' bias in surface temperature trends and variability. Environmental Research Letters 9, (2014).
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).
Diurnal asymmetry to the observed global warming. International Journal of Climatology (2015).
Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth. Nature Communications 7, (2016).
Complementary explanation of temperature response in the lower atmosphere. Environmental Research Letters 7, (2012).
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).
The Climatology of the Atmospheric Boundary Layer in Contemporary Global Climate Models. Journal of Climate 31, (2018).
