Biblio
Filters: Author is Davy, Richard [Clear All Filters]
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).
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).
Micro-climate on MEGA-computers. META (2012).
Complementary explanation of temperature response in the lower atmosphere. Environmental Research Letters 7, (2012).
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 and Sustainable Energy Reviews 81, (2017).
Reconciling high resolution climate datasets using KrigR. Environmental Research Letters 16, (2021).
The Arctic Surface Climate in CMIP6: Status and Developments since CMIP5. Journal of Climate 33, (2020).
Diurnal asymmetry to the observed global warming. International Journal of Climatology (2015).
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). Download: davy_2014_global_climate_models_bias_in_surface_temperature_trends_and_variability.pdf (2.02 MB)
Surface air temperature variability in global climate models. Atmospheric Science Letters 15, (2014). Abstract
Download: davy_esau_2014_surface_air_temperature_variability_in_global_climate_models.pdf (472.83 KB)
Surface air temperature changes in the high-latitude boundary layer. Report Series in Aerosol Science 180, (2016).
Differences in the efficacy of climate forcings explained by variations in atmospheric boundary layer depth. Nature Communications 7, (2016).
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
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).
