Biblio
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Driving Mechanisms of an Extreme Winter Sea Ice Breakup Event in the Beaufort Sea. Geophysical Research Letters 49, (2022).
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).
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).
Climate change impacts on wind energy potential in the European domain with a focus on the Black Sea. Renewable and Sustainable Energy Reviews 81, (2017).
Atmospheric heat advection in the Kara Sea region under main synoptic processes. International Journal of Climatology 39, (2018).
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).
The Arctic Surface Climate in CMIP6: Status and Developments since CMIP5. Journal of Climate 33, (2020).
Arctic Sea-Level Change in Remote Sensing and New Generation Climate Models. Advances in Remote Sensing Technology and the Three Poles (2022).doi:10.1002/9781119787754
Anthropogenic heating strongly amplifies the urban heat island in Arctic cities. Atmospheric Chemistry and Physics (ACP) 18, (2018).
Anthropogenic and natural drivers of a strong winter urban heat island in a typical Arctic city. Atmospheric Chemistry and Physics (ACP) 18, (2018).