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From aerosol-limited to invigoration of warm convective clouds

Science (American Association for the Advancement of Science), 2014-06, Vol.344 (6188), p.1143-1146

2014

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Distinct Mixing Regimes in Shallow Cumulus Clouds

Geophysical research letters, 2024-01, Vol.51 (2), p.n/a

2024

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Cloud Versus Void Chord Length Distributions (LvL) as a Measure for Cloud Field Organization

Geophysical research letters, 2024-06, Vol.51 (11), p.n/a

2024

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Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans

Scientific reports, 2019-05, Vol.9 (1), p.7809-7809, Article 7809

2019

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Aerosol effects on the timing of warm rain processes

Geophysical research letters, 2015-06, Vol.42 (11), p.4590-4598

2015

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Quantifying the effect of aerosol on vertical velocity and effective terminal velocity in warm convective clouds

Atmospheric chemistry and physics, 2018-05, Vol.18 (9), p.6761-6769

2018

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Diel cycle of sea spray aerosol concentration

Nature communications, 2021-09, Vol.12 (1), p.5476-5476, Article 5476

2021

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Aerosol effect on the mobility of cloud droplets

Environmental research letters, 2015-10, Vol.10 (10), p.104011

2015

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How do changes in warm-phase microphysics affect deep convective clouds?

Atmospheric chemistry and physics, 2017-08, Vol.17 (15), p.9585-9598

2017

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Observed decreasing trend in the upper-tropospheric cloud top temperature

NPJ climate and atmospheric science, 2023-09, Vol.6 (1), p.142-8, Article 142

2023

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Global association of aerosol with flash density of intense lightning

Environmental research letters, 2017-11, Vol.12 (11), p.114037

2017

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Shallow Convective Cloud Field Lifetime as a Key Factor for Evaluating Aerosol Effects

iScience, 2018-12, Vol.10, p.192-202

2018

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Characterization of cumulus cloud fields using trajectories in the center of gravity versus water mass phase space: 2. Aerosol effects on warm convective clouds

Journal of geophysical research. Atmospheres, 2016-06, Vol.121 (11), p.6356-6373

2016

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Aerosol effects on the inter-cloud region of a small cumulus cloud field

Geophysical research letters, 2009-07, Vol.36 (14), p.L14805-n/a

2009

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Enhanced humidity pockets originating in the mid boundary layer as a mechanism of cloud formation below the lifting condensation level

Environmental research letters, 2017-02, Vol.12 (2), p.24020

2017

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Oscillations in deep-open-cells during winter Mediterranean cyclones

NPJ climate and atmospheric science, 2021-03, Vol.4 (1), p.1-7, Article 12

2021

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On the properties and radiative effects of small convective clouds during the eastern Mediterranean summer

Environmental research letters, 2015-04, Vol.10 (4), p.44006

2015

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On the signature of the cirrus twilight zone

Environmental research letters, 2014-09, Vol.9 (9), p.94010

2014

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Convective Steady State in Shallow Cloud Fields

Physical review letters, 2023-09, Vol.131 (13), p.134201-134201, Article 134201

2023

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Simulation of the electrification of winter thunderclouds using the three-dimensional Regional Atmospheric Modeling System (RAMS) model: Single cloud simulations

Journal of Geophysical Research - Atmospheres, 2005-10, Vol.110 (D20), p.D20205-n/a

2005

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Shallow Cumulus Properties as Captured by Adiabatic Fraction in High-Resolution LES Simulations

Journal of the atmospheric sciences, 2022-02, Vol.79 (2), p.409-428

2022

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Lightning activity over land and sea on the eastern coast of the Mediterranean

Monthly weather review, 2003-09, Vol.131 (9), p.2060-2070

2003

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Opposing trends of cloud coverage over land and ocean under global warming

Atmospheric chemistry and physics, 2023-06, Vol.23 (11), p.6559-6569

2023

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Uncovering the Large‐Scale Meteorology That Drives Continental, Shallow, Green Cumulus Through Supervised Classification

Geophysical research letters, 2022-04, Vol.49 (8), p.e2021GL096684-n/a

2022

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Convective and turbulent motions in non-precipitating Cu. Part 1: Method of separation of convective and turbulent motions

Journal of the atmospheric sciences, 2021-01, Vol.78 (7)

2021

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From aerosol-limited to invigoration of warm convective clouds

Distinct Mixing Regimes in Shallow Cumulus Clouds

Cloud Versus Void Chord Length Distributions (LvL) as a Measure for Cloud Field Organization

Non-Monotonic Aerosol Effect on Precipitation in Convective Clouds over Tropical Oceans

Aerosol effects on the timing of warm rain processes

Quantifying the effect of aerosol on vertical velocity and effective terminal velocity in warm convective clouds

Diel cycle of sea spray aerosol concentration

Aerosol effect on the mobility of cloud droplets

How do changes in warm-phase microphysics affect deep convective clouds?

Observed decreasing trend in the upper-tropospheric cloud top temperature

Global association of aerosol with flash density of intense lightning

Shallow Convective Cloud Field Lifetime as a Key Factor for Evaluating Aerosol Effects

Characterization of cumulus cloud fields using trajectories in the center of gravity versus water mass phase space: 2. Aerosol effects on warm convective clouds

Aerosol effects on the inter-cloud region of a small cumulus cloud field

Enhanced humidity pockets originating in the mid boundary layer as a mechanism of cloud formation below the lifting condensation level

Oscillations in deep-open-cells during winter Mediterranean cyclones

On the properties and radiative effects of small convective clouds during the eastern Mediterranean summer

On the signature of the cirrus twilight zone

Convective Steady State in Shallow Cloud Fields

Simulation of the electrification of winter thunderclouds using the three-dimensional Regional Atmospheric Modeling System (RAMS) model: Single cloud simulations

Shallow Cumulus Properties as Captured by Adiabatic Fraction in High-Resolution LES Simulations

Lightning activity over land and sea on the eastern coast of the Mediterranean

Opposing trends of cloud coverage over land and ocean under global warming

Uncovering the Large‐Scale Meteorology That Drives Continental, Shallow, Green Cumulus Through Supervised Classification

Convective and turbulent motions in non-precipitating Cu. Part 1: Method of separation of convective and turbulent motions

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