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Cloud albedo
Aerosol Effective Radiative Forcing in the Online Aerosol Coupled CAS
Marine Cloud Brightening
Estimation of Cloud Condensation Nuclei Concentration from Aerosol Optical Quantities: Influential Factors and Uncertainties
Aerosols, Their Direct and Indirect Effects
ALBEDO ENHANCEMENT by STRATOSPHERIC SULFUR INJECTIONS: a CONTRIBUTION to RESOLVE a POLICY DILEMMA? an Editorial Essay
Oceanic Phytoplankton, Atmospheric Sulphur, Cloud Albedo and Climate Robert J
Earth Energy Budget and Balance
Development of a Scheme for Parameterizing the Effects of Cloud Condensation Nuclei on Stratocumulus Cloud Albedo
Cloud Condensation Nuclei (CCN) Properties of Ambient Aerosol
Solar Radiance and Albedo of Clouds from Space Lidar
Retrievals of Cloud Fraction and Cloud Albedo from Surfacebased
Simultaneous Observations of Aerosol–Cloud–Albedo Interactions with Three Stacked Unmanned Aerial Vehicles
Pollution and the Planetary Albedo
Constraining the Instantaneous Aerosol Influence on Cloud Albedo
Energy Budget
Marine Cloud Brightening: Science, Feasibility and a Plan for Research
Fighting Climate Change by Engineering Air Pollution to Brighten Clouds Lynn Russell, Scripps Institution of Oceanography
Global Cloud Condensation Nuclei Influenced by Carbonaceous
Top View
The Atmospheric Aerosols and Their Effects on Cloud Albedo and Radiative Forcing
UNIVERSITY of CALIFORNIA, SAN DIEGO Observational Estimates Of
Are Global Cloud Albedo and Climate Controlled by Marine Phytoplankton? Stephen E
Cloud Albedo Changes in Response to Anthropogenic Sulfate and Non-Sulfate Aerosol Forcings in CMIP5 Models
Cloud Albedo Can Generally Be Parameterized by Optical Depth And
MERIS Cloud Albedo and Cloud Optical Thickness Algorithm
The Role of the Effective Cloud Albedo for Climate Monitoring and Analysis
Response to Marine Cloud Brightening in a Multi-Model Ensemble
Transmission of Solar Radiation by Clouds Over Snow and Ice Surfaces: a Parameterization in Terms of Optical Depth, Solar Zenith Angle, and Surface Albedo
Impacts of Aerosol Particles on the Microphysical and Radiative
Climate Radiative Forcing of Gases, Aerosols, and Clouds. Part 3. Objectives: 1
Why Is the Cloud Albedo - Particle Size Relationship Different in Optically Thick and Optically Thin Clouds?
Marine Cloud Brightening – As Effective Without Clouds
Using Two-Stream Theory to Capture Fluctuations of Satellite-Perceived
Impact of Aerosols on the Hydrological Cycle
Factors Determining the Most Efficient Spray Distribution for Marine Cloud
Relationship Between Cloud Radiative Forcing, Cloud Fraction and Cloud Albedo, and New Surface-Based Approach for Determining Cloud Albedo
Reduced Efficacy of Marine Cloud Brightening Geoengineering Due To
Energy Budget
Geoengineering: Impact of Marine Cloud Brightening Control on the Extreme Temperature Change Over East Asia
Climate Impacts of Marine Cloud Brightening
(SESORA) Forecast for Solar Surface Irradiance—Method and Validation