Evaporation and condensation of water mist/cloud droplets with thermal radiation

Keyphrases

• Condensation 100%
• Response Surface Regression 100%
• Thermal Radiation 100%
• Advection 100%
• Cloud Droplets 100%
• Water Mist 100%
• Ambient Conditions 50%
• Kohler 50%
• Supersaturation 50%
• Non-continuum 50%
• Evaporation Rate 50%
• Lower Limit 50%
• Missing Data Mechanism 50%
• Liquid Phase 50%
• Diffusional 50%
• Infrared Absorption 50%
• Infrared Emission 50%
• Droplet Size 50%
• Isothermal Condition 50%
• Gas-liquid 50%
• Evaporative 50%
• Solar Radiation 50%
• Droplet Size Distribution 50%
• Comparison with Experimental Results 50%
• Droplet Growth 50%
• Depth Effect 50%
• Liquid Velocity 50%
• Nonradiating 50%
• Upper Layer 50%
• Large Droplets 50%
• Condensational Growth 50%
• Gas Effect 50%
• Lower Layer 50%
• Surface Phenomena 50%
• Coalescence Growth 50%
• Water Droplet Evaporation 50%
• Ground Radiation 50%
• Velocity Slip Effect 50%
• Droplet Condensation 50%
• Droplet Stability 50%
• Thermal Radiation Effects 50%
• Warm Rain 50%
• Rain Droplets 50%
• Cloud Droplet Growth 50%
• Equilibrium Droplets 50%

Engineering

• Thermal Radiation 100%
• Cloud Droplet 100%
• Advection 66%
• Droplet Growth 66%
• Ambient Condition 33%
• Isothermal 33%
• Experimental Result 33%
• Radiation Effect 33%
• Supersaturation 33%
• Upper Limit 33%
• Evaporation Rate 33%
• Infrared Absorption 33%
• Droplet Size 33%
• Isothermal Condition 33%
• Liquid Phase 33%
• Lower Limit 33%
• Solar Radiation 33%
• Liquid Velocity 33%
• Droplet Size Distribution 33%