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What sets aeolian dune height?

Nature communications, 2022-05, Vol.13 (1), p.2401-2401, Article 2401

2022

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Flux–Profile Relationships in the Stable Boundary Layer—A Critical Discussion

Atmosphere, 2021-09, Vol.12 (9), p.1197

2021

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The Boundary Layer Air Quality-Analysis Using Network of Instruments (BAQUNIN) Supersite for Atmospheric Research and Satellite Validation over Rome Area

Bulletin of the American Meteorological Society, 2022-02, Vol.103 (2), p.E599-E618

2022

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Future Climate Change Impact on Urban Heat Island in Two Mediterranean Cities Based on High-Resolution Regional Climate Simulations

Atmosphere, 2021-07, Vol.12 (7), p.884

2021

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Turbulence, Low-Level Jets, and Waves in the Tyrrhenian Coastal Zone as Shown by Sodar

Atmosphere, 2020-01, Vol.11 (1), p.28

2020

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Genomic and physiological resilience in extreme environments are associated with a secure attachment style

Translational psychiatry, 2020-06, Vol.10 (1), p.185, Article 185

2020

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Surface and Aerodynamic Parameters Estimation for Urban and Rural Areas

Atmosphere, 2020-02, Vol.11 (2), p.147

2020

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Beer–Lambert law in photochemistry: A new approach

Journal of photochemistry and photobiology. A, Chemistry., 2022-11, Vol.432, p.114086, Article 114086

2022

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Large aerosol effects on ozone photolysis in the Mediterranean

Atmospheric environment (1994), 2011-08, Vol.45 (24), p.3937-3943

2011

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Mini Neutron Monitors at Concordia Research Station, Central Antarctica

Journal of astronomy and space sciences, 2015-12, Vol.32 (4), p.281-287

2015

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On the application of Mittag–Leffler functions to hyperbolic-type decay of luminescence

The Journal of physics and chemistry of solids, 2022-04, Vol.163, p.110538, Article 110538

2022

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Stable Surface-Based Turbulent Layer During the Polar Winter at Dome C, Antarctica: Sodar and In Situ Observations

Boundary-layer meteorology, 2019-04, Vol.171 (1), p.101-128

2019

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Seasonal variability of tropospheric aerosols in Rome

Atmospheric research, 2012-11, Vol.118, p.205-214

2012

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The surface layer observed by a high-resolution sodar at DOME C, Antarctica

Annals of geophysics, 2013-01, Vol.56 (5)

2013

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Measuring the urban heat island of Rome through a dense weather station network and remote sensing imperviousness data

Urban climate, 2023-01, Vol.47, p.101355, Article 101355

2023

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Towards a Generalized Beer-Lambert Law

Fractal and fractional, 2018-03, Vol.2 (1), p.8

2018

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Interaction of the Sea Breeze with the Urban Area of Rome: WRF Mesoscale and WRF Large-Eddy Simulations Compared to Ground-Based Observations

Boundary-layer meteorology, 2022-12, Vol.185 (3), p.333-363

2022

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Kelvin–Helmholtz Billows in the Rising Turbulent Layer During Morning Evolution of the ABL at Dome C, Antarctica

Boundary-layer meteorology, 2023-05, Vol.187 (1-2), p.163-192

2023

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Sensitivity of near-surface meteorology to PBL schemes in WRF simulations in a port-industrial area with complex terrain

Atmospheric research, 2021-12, Vol.264, p.105824, Article 105824

2021

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Momentum- and Heat-Flux Parametrization at Dome C, Antarctica: A Sensitivity Study

Boundary-layer meteorology, 2017-02, Vol.162 (2), p.341-367

2017

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Observed and Modelled Convective Mixing-Layer Height at Dome C, Antarctica

Boundary-layer meteorology, 2014-06, Vol.151 (3), p.597-608

2014

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Quantitative Interpretation of Air Radon Progeny Fluctuations in Terms of Stability Conditions in the Atmospheric Boundary Layer

Boundary-layer meteorology, 2016-09, Vol.160 (3), p.529-550

2016

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Assessing the Departures from the Energy- and Flux-Budget (EFB) Model in Heterogeneous and Urbanized Environment for Stable Atmospheric Stratification

Boundary-layer meteorology, 2023-05, Vol.187 (1-2), p.339-369

2023

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Wavelike Structures in the Turbulent Layer During the Morning Development of Convection at Dome C, Antarctica

Boundary-layer meteorology, 2016-11, Vol.161 (2), p.289-307

2016

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Stable boundary‐layer regimes at Dome C, Antarctica: observation and analysis

Quarterly journal of the Royal Meteorological Society, 2017-04, Vol.143 (704), p.1241-1253

2017

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What sets aeolian dune height?

Flux–Profile Relationships in the Stable Boundary Layer—A Critical Discussion

The Boundary Layer Air Quality-Analysis Using Network of Instruments (BAQUNIN) Supersite for Atmospheric Research and Satellite Validation over Rome Area

Future Climate Change Impact on Urban Heat Island in Two Mediterranean Cities Based on High-Resolution Regional Climate Simulations

Turbulence, Low-Level Jets, and Waves in the Tyrrhenian Coastal Zone as Shown by Sodar

Genomic and physiological resilience in extreme environments are associated with a secure attachment style

Surface and Aerodynamic Parameters Estimation for Urban and Rural Areas

Beer–Lambert law in photochemistry: A new approach

Large aerosol effects on ozone photolysis in the Mediterranean

Mini Neutron Monitors at Concordia Research Station, Central Antarctica

On the application of Mittag–Leffler functions to hyperbolic-type decay of luminescence

Stable Surface-Based Turbulent Layer During the Polar Winter at Dome C, Antarctica: Sodar and In Situ Observations

Seasonal variability of tropospheric aerosols in Rome

The surface layer observed by a high-resolution sodar at DOME C, Antarctica

Measuring the urban heat island of Rome through a dense weather station network and remote sensing imperviousness data

Towards a Generalized Beer-Lambert Law

Interaction of the Sea Breeze with the Urban Area of Rome: WRF Mesoscale and WRF Large-Eddy Simulations Compared to Ground-Based Observations

Kelvin–Helmholtz Billows in the Rising Turbulent Layer During Morning Evolution of the ABL at Dome C, Antarctica

Sensitivity of near-surface meteorology to PBL schemes in WRF simulations in a port-industrial area with complex terrain

Momentum- and Heat-Flux Parametrization at Dome C, Antarctica: A Sensitivity Study

Observed and Modelled Convective Mixing-Layer Height at Dome C, Antarctica

Quantitative Interpretation of Air Radon Progeny Fluctuations in Terms of Stability Conditions in the Atmospheric Boundary Layer

Assessing the Departures from the Energy- and Flux-Budget (EFB) Model in Heterogeneous and Urbanized Environment for Stable Atmospheric Stratification

Wavelike Structures in the Turbulent Layer During the Morning Development of Convection at Dome C, Antarctica

Stable boundary‐layer regimes at Dome C, Antarctica: observation and analysis

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