Results 81 to 90 of about 8,818 (209)
Large‐eddy simulation (LES) of clouds has the potential to resolve a central question in climate dynamics, namely, how subtropical marine boundary layer (MBL) clouds respond to global warming.
Zhihong Tan +3 more
doaj +1 more source
Abstract The response of marine low‐cloud mesoscale morphologies to climate change and emission reductions remains poorly understood. Here, we link long‐term trends in six cloud morphologies to variations in large‐scale meteorology and aerosols. The trends show strong spatial heterogeneity, with closed and disorganized mesoscale cellular convection ...
Jihu Liu +7 more
wiley +1 more source
Importance of composition and hygroscopicity of BC particles to the effect of BC mitigation on cloud properties: Application to California conditions [PDF]
Black carbon (BC) has many effects on climate including the direct effect on atmospheric absorption, indirect and semi-direct effects on clouds, snow effects, and others.
Adams, Peter +6 more
core +1 more source
Abstract The radiative effect of aerosol on cloud albedo via altering cloud droplet effective radius (re) is a major uncertainty in the Earth's climate system. Remote sensing studies have reported either negative or positive relationships between re and aerosol number concentration (Na) or other aerosol proxies.
Jiannong Quan +7 more
wiley +1 more source
On the relationship between responses in cloud water and precipitation to changes in aerosol [PDF]
Climate models continue to exhibit strong sensitivity to the representation of aerosol effects on cloud reflectance and cloud amount. This paper evaluates a proposed method to constrain modeled cloud liquid water path (LWP) adjustments in response to ...
Z. J. Lebo, G. Feingold
doaj +1 more source
Low Cloud Dispersion Effects by Anthropogenic Aerosols in Polluted Air
Abstract Aerosol–cloud interactions (ACI) are a major source of uncertainty in anthropogenic climate forcing. Anthropogenic aerosols modulate the cloud albedo by impacting the relative dispersion (ε) of cloud droplet size distributions (CDSDs), known as the dispersion effect.
Xiaomi Teng +13 more
wiley +1 more source
Kernel‐Based Estimation of Stratospheric Aerosol Radiative Effects From Volcanic and Wildfire Events
Abstract To facilitate the quantification of the stratospheric aerosol direct radiative effect (ARE), this study develops a suite of aerosol kernels based on Modern‐Era Retrospective Analysis for Research and Applications, Version 2 reanalysis data. The kernels comprise a five‐dimensional data set that includes latitude, longitude, time, wavelength ...
Qiurun Yu, Yi Huang
wiley +1 more source
Resolving Droplet Sedimentation Effects in Stratocumulus Clouds
AbstractWe use direct numerical simulations to quantify the effects that droplet sedimentation has on the stratocumulus‐topped boundary layer. Our analysis includes both ends of the length‐scale spectrum that are deemed important for representing turbulence in stratocumulus clouds, spanning from meter scales at the cloud top to large energy‐containing ...
Raphael Pistor, Juan Pedro Mellado
openaire +2 more sources
Biases in Southern Ocean Precipitation From Shallow Convection: The Role of Cloud Morphology
Abstract Precipitation from marine boundary layer clouds is a critical yet highly uncertain feature of post‐frontal conditions over the Southern Ocean (SO), where shallow convection dominates. This study evaluates whether satellite retrievals (GPM‐IMERG and CloudSat) and reanalysis (ERA5) represent the contrasting precipitation between open and closed ...
T. Alinejadtabrizi +6 more
wiley +1 more source
Abstract Mixed‐phase clouds modulate the water and energy cycles of high‐latitude regions, yet their liquid‐ice phase partitioning has long been poorly simulated in climate models. Here, simulations of Arctic mixed‐phase clouds by the Simple Cloud‐Resolving E3SM Atmosphere Model (SCREAM) are assessed against large‐eddy simulations, satellite data, and ...
Lin Lin +7 more
wiley +1 more source

