Results 191 to 200 of about 63,736 (296)

Contribution of Satellite-Derived Aerosol Optical Depth PM_2.5 Bayesian Concentration Surfaces to Respiratory-Cardiovascular Chronic Disease Hospitalizations in Baltimore, Maryland. [PDF]

Atmosphere (Basel), 2020
Braggio JT, Hall ES, Weber SA, Huff AK.
europepmc   +1 more source

Satellite Observations Show Negligible Impact of Mineral Dust on Cloud Droplet Number

Geophysical Research Letters, Volume 53, Issue 5, 16 March 2026.
Abstract The susceptibility of cloud droplet number concentration Nd $\left({N}_{\mathrm{d}}\right)$ to aerosols (β) $(\beta )$ remains challenging to constrain in satellite observations. This difficulty arises from limitations in representing cloud condensation nuclei, which depend on aerosol size and composition.
Goutam Choudhury, Tom Goren, Matthias Tesche   +2 more
wiley   +1 more source

Comparative analysis of CAMS aerosol optical depth data and AERONET observations in the Eastern Mediterranean over 19 years. [PDF]

Environ Sci Pollut Res Int
Tuna Tuygun G, Elbir T.
europepmc   +1 more source

Evaluating the Impact of Assimilating Aerosol Optical Depth Observations on Dust Forecasts Over North Africa and the East Atlantic Using Different Data Assimilation Methods. [PDF]

J Adv Model Earth Syst, 2020
Choi Y, Chen SH, Huang CC, Earl K, Chen CY, Schwartz CS, Matsui T.   +6 more
europepmc   +1 more source

CNN‐Based Retrieval of 3D Cloud Structures Solely From Geostationary Satellite Imagery

Geophysical Research Letters, Volume 53, Issue 5, 16 March 2026.
Abstract The cloud vertical structure (CVS) is important, yet operational CVS products depend on active observation or reanalysis fields, limiting high‐frequency monitoring. In this study, we propose a lightweight and satellite‐only model that reconstructs volumetric cloud masks from geostationary multispectral imagery.
Chi Yang, Fu Wang, Qifeng Lu, Ruixia Liu, Xiaofei Yang, Jiaxin Cheng, Yong Cao, Zhuoya Ni   +7 more
wiley   +1 more source

Influence of COVID-19 Lockdown on Aerosol Optical Depth over Pokhara and Kyanjin Gompa in Nepal

, 2021
Silwal A, Gautam SP, Karki M, Poudel P, Thapa A, Chapagain NP, Adhikari B.   +6 more
europepmc   +1 more source

Surface Observations From Atmospheric Radiation Measurement Sites Constrain the Anthropogenic Contribution to Cloud Droplet Number

Geophysical Research Letters, Volume 53, Issue 5, 16 March 2026.
Abstract Uncertainty in anthropogenic forcing driven by aerosol‐cloud interactions (aci) limits our ability to infer the sensitivity of the Earth system to forcing from historical records. The driver of aci is the change in cloud droplet number concentration (Nd) due to changes in aerosol serving as cloud condensation nuclei (CCN).
Dani B. Jones, Hunter Y. Brown, Jacqueline M. Nugent, August Mikkelsen, Ci Song, Damao Zhang, Susannah M. Burrows, Hamish Gordon, Andrew Kirby, Daniel T. McCoy   +9 more
wiley   +1 more source

Interconnection of Aerosol‐Cloud Interactions and Cloud Feedback Through Warm Rain Process

Journal of Geophysical Research: Atmospheres, Volume 131, Issue 5, 16 March 2026.
Abstract Recent research has revealed a correlation within the Coupled Model Intercomparison Project Phase 6 (CMIP6) simulations: models exhibiting more pronounced warming due to positive cloud feedback simultaneously show enhanced cooling from aerosol‐cloud interactions (ACI).
Chuan Feng, Xiaohong Liu, Xi Zhao, Zheng Lu, Lin Lin, Mark D. Zelinka, Yi Qin, Yunpeng Shan, Youtong Zheng, Xingru Wu, Ramalingam Saravanan   +10 more
wiley   +1 more source

Improving Dust Aerosol Optical Depth (DAOD) Retrieval from the GEOKOMPSAT-2A (GK-2A) Satellite for Daytime and Nighttime Monitoring. [PDF]

Sensors (Basel)
Ahn S, Kim HS, Byon JY, Lim H.
europepmc   +1 more source

Ratios of Extinction Coefficient, Mass, and Surface Area to Backscatter Coefficient and Mass to Extinction Coefficient Derived From Balloon‐Borne Stratospheric Aerosol Size Distribution Measurements From 1989–2025

Journal of Geophysical Research: Atmospheres, Volume 131, Issue 5, 16 March 2026.
Abstract In situ measurements of stratospheric aerosol are the only measurements that provide sufficient detail to determine aerosol number, size, surface area, volume/mass, and effective radius; however, these measurements are limited in space and time.
Terry Deshler, Lars E. Kalnajs
wiley   +1 more source