Journal of Atmospheric and Solar-Terrestrial Physics, Journal Year: 2024, Volume and Issue: unknown, P. 106411 - 106411
Published: Dec. 1, 2024
Language: Английский
Journal of Atmospheric and Solar-Terrestrial Physics, Journal Year: 2024, Volume and Issue: unknown, P. 106411 - 106411
Published: Dec. 1, 2024
Language: Английский
Geophysical Research Letters, Journal Year: 2025, Volume and Issue: 52(7)
Published: March 31, 2025
Abstract Relative dispersion ( ε ), as a parameter characterizing droplet spectral shape, exerts considerable impact on cloud radiation and precipitation processes, its accurate parameterization is urgently needed in models. Current parameterizations, which are based number concentration or simply set constants, inadequate to satisfy the demand. This study shows, utilizing in‐situ fog observations from five underlying surface regions (urban, suburban, mountainous, coastal rainforest) of China, that uniformly stably manifests initially increasing then decreasing volume‐mean diameter increases across these regions. Based this relationship, established, exhibits improved predictive capabilities evaluating both albedo effect lifetime effect. The expected enhance simulation accuracy minimize discrepancy between observed simulated precipitation, particularly for weather climate models commonly use double‐moment microphysical schemes.
Language: Английский
Citations
1Geophysical Research Letters, Journal Year: 2024, Volume and Issue: 51(19)
Published: Oct. 1, 2024
Abstract The influence of entrainment, a key process characterized by the entrainment rate in cumulus parameterization, on aerosol‐cloud interactions has been widely recognized. However, despite qualitative links established between and aerosol loading, quantitative relationship based observational evidence remains elusive. This study utilizes aircraft observations clouds during two field campaigns to determine loading. In both campaigns, is negatively correlated with It speculated that increased loading enhances cloud edge droplet evaporation, which leads buoyancy vertical velocity within cloud, thereby reducing rate. Further analysis shows response perturbations more significant smaller weak less pronounced under opposite conditions. These findings shed new light improving description parameterizations.
Language: Английский
Citations
5Atmospheric Research, Journal Year: 2025, Volume and Issue: unknown, P. 107994 - 107994
Published: Feb. 1, 2025
Language: Английский
Citations
0Proceedings of the National Academy of Sciences, Journal Year: 2025, Volume and Issue: 122(13)
Published: March 24, 2025
The Twomey effect brightens clouds by increasing aerosol concentrations, which activates more droplets and decreases cloud supersaturation in response to competition for water vapor. To quantify this response, we used marine low observations clean smoky conditions at Ascension Island the tropical South Atlantic during Layered Aerosol Smoke Interactions with Cloud (LASIC) campaign. These show similar increases droplet number increased accumulation-mode particles from surface-based satellite retrievals, demonstrating importance of below-cloud measurements retrieving aerosol–cloud interactions (ACI) conditions. Four methods estimating were compared, scene-based parcel-based showing sufficient variability a strong dependence on both accumulation concentration cloud-base updraft velocities. Decomposing aerosol-related changes albedo optical depth shows calculated accounts dampening activation 12 35%, explaining diminished high concentrations observed LASIC previously around world. This result was consistent independent retrievals condensation nuclei multimode size-resolving Lagrangian methods. Translating effects local radiative forcing as proxy preindustrial present-day showed that reduces cooling providing an essential process-specific constraint improving representation climate model simulation indirect forcing.
Language: Английский
Citations
0Journal of Geophysical Research Atmospheres, Journal Year: 2024, Volume and Issue: 129(17)
Published: Sept. 4, 2024
Abstract The study on the characteristic and parameterization of cloud droplet effective radius ( r e ) is important for optimization warm microphysical schemes in numerical models. Based simulations combined with four aircraft observations stratiform clouds Jiangxi, China, this work investigated their properties, focusing evolutionary pattern , as well correlation between number concentration N c liquid water path (LWP). It found that there a negative rate decrease could be increased by 2–4 times strengthening collision‐coalescence process. What's more, direct introduction conducted based existing schemes, results show it can perform most intensities. also LWP positively correlated when less than 12 μm, after which relationship changes to due impact rainfall intensity.
Language: Английский
Citations
0Atmospheric chemistry and physics, Journal Year: 2024, Volume and Issue: 24(23), P. 13525 - 13540
Published: Dec. 9, 2024
Abstract. Changes in aerosol amount and size distribution significantly impact cloud droplet distribution, as aerosols act condensation nuclei (CCNs) influence the relative dispersion (ε) of spectra. Relative plays a key role parameterizing processes general circulation models (GCMs) microphysical schemes, affecting precipitation estimates climate predictions. However, effects varying modes on microphysics remain debated, depending thermodynamic conditions type. This study simulates warm stratiform Jiangxi, China, using Weather Research Forecasting (WRF) Spectra–Bin Microphysics scheme (SBM-FAST) from 18:00 24 December 2014 to 06:00 25 (UTC). Satellite aircraft observations were used validate simulation, showing good agreement structure. Sensitivity experiments conducted by increasing nucleation, accumulation, coarse-mode 5-fold reducing total concentration 1/5 control. Results show that higher concentrations enhance formation broaden spectra, while lower suppress development. Accumulation-mode increase small-droplet concentrations, nucleation- favor larger droplets. The correlation between ε volume-weighted radius (Rv) shifts positive negative Rv increases. transition is driven collision–coalescence, condensation, activation. Increased accumulation-mode shift ε–Rv range 4.5–8 µm, reduced strengthen correlation. Regardless different coalescence intensities, converges with number droplets (Nc).
Language: Английский
Citations
0Atmospheric Research, Journal Year: 2024, Volume and Issue: 315, P. 107881 - 107881
Published: Dec. 22, 2024
Language: Английский
Citations
0Journal of Atmospheric and Solar-Terrestrial Physics, Journal Year: 2024, Volume and Issue: unknown, P. 106411 - 106411
Published: Dec. 1, 2024
Language: Английский
Citations
0