Results 141 to 150 of about 24,097 (273)
Transport to the Extratropical Stratosphere by Overshooting Storms in Idealized Simulations
Abstract Deep convection is a significant source of water to the extratropical stratosphere which can alter radiative properties and contribute to ozone loss. Previous studies find it responsible for 40% of mid‐latitude water vapor above 380K. However, the amount of hydration from individual storms and the mechanisms that initiate mixing is less ...
Devin P. Bissell +3 more
wiley +1 more source
Microphysics of Clouds and Precipitation [PDF]
Hans R. Pruppacher +2 more
openaire +1 more source
Atmospheric Adjustments to In Situ Cirrus Formation in Ice Supersaturated Regions
Abstract High‐level ice clouds exert a net warming on the climate system because their greenhouse effect outweighs their albedo effect. Focusing on in‐situ cirrus, their formation involves the conversion of upper‐tropospheric water vapor into ice crystals.
Jérémie Juvin‐Quarroz +5 more
wiley +1 more source
Data-driven emulation of modal aerosol microphysics via neural operator-based modeling. [PDF]
Bai Z, Rouson D.
europepmc +1 more source
Abstract Fogs formed by aerosol activation in supersaturated air often cause extremely poor visibility, yet accurate prediction remains challenging and models typically account for only fog droplet extinction. The role of fog interstitial aerosols has remained largely unexplored due to limited observational capabilities.
Weihong Huang +14 more
wiley +1 more source
Long-Term Impact of Urban Areas on Meteorological Conditions Over Central Europe. [PDF]
Villalba-Pradas A +4 more
europepmc +1 more source
Network Divergence Reveals Predictable Pathways of Extreme Rainfall in Central India
Abstract Extreme rainfall events over Central India have increased, reflecting intensified monsoon precipitation driven by factors like urbanization and land use change. With projections indicating further intensification and flood vulnerability, better prediction is critical.
Akash Singh Raghuvanshi, Ankit Agarwal
wiley +1 more source
Generating a stratocumulus-like cloud top in a convection-cloud chamber. [PDF]
Wang A +4 more
europepmc +1 more source
Abstract The primary uncertainty in anthropogenic climate forcing arises from a limited understanding of aerosol effects on cloud albedo, which in combination with other effects, is termed the radiative forcing from aerosol‐cloud interactions (RFaci).
Lan Gao +13 more
wiley +1 more source
Vertical motions in clouds from EarthCare satellite and a global storm-resolving modeling. [PDF]
Roh W +5 more
europepmc +1 more source

