Not as random: the stable dynamics controlling shallow convective clouds. [PDF]
Koren I, Dror T, Shehter ER, Altaratz O.
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Observational Assessment of Changes in Earth's Energy Imbalance Since 2000. [PDF]
Loeb NG +7 more
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Detectable ship tracks account for just 5% of aerosol indirect forcing from ship emissions. [PDF]
Yuan T, Song H, Boss LF, Diamond MS.
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Solar geoengineering may not prevent strong warming from direct effects of CO2 on stratocumulus cloud cover. [PDF]
Schneider T, Kaul CM, Pressel KG.
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Severe turbulence from deep convective clouds during flight SQ321 on 21 May 2024. [PDF]
Wang KY.
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Reduced aerosol pollution diminished cloud reflectivity over the North Atlantic and Northeast Pacific. [PDF]
von Salzen K +8 more
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Competition response of cloud supersaturation explains diminished Twomey effect for smoky aerosol in the tropical Atlantic. [PDF]
Dedrick JL +5 more
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Recent Advances in the Observation and Modeling of Aerosol-Cloud Interactions, Cloud Feedbacks, and Earth's Energy Imbalance: A Review. [PDF]
Michibata T +4 more
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Removal of trace gases can both increase and decrease cloud droplet formation. [PDF]
Ravichandran E +11 more
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Less anthropogenic aerosol indirect effects are a potential cause for Northeast Pacific warm blob events. [PDF]
Yao N +7 more
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