Growth rate measurements were made for water drops grown on nuclei in atmospheric air samples taken in Rolla, Missouri. Rolla, having a population of 15,000 and very little industry, is relatively free of urban pollutants. The measurements were made in a vertical flow thermal diffusion chamber at supersaturations of 0. 5 and 1%. The time to grow from near dry radius to the final radius (6 to 7. 5 mu m) was measured. If one assumes the thermal accomodation coefficient is unity, the measurements indicate an average value of 0. 026 for the condensation coefficient. The temperature ranged from 22. 5 to 25. 7 degree C
Dropwise condensation of atmospheric water vapor is important in multiple practical engineering appl...
A pulse-expansion wave tube method to determine homogeneous nucleation rates of water droplets has b...
Measurements of cloud condensation nuclei (CCN) concentrations (cm -3) between 0.2 and 1.0% supersat...
Values of condensation coefficient, ß, were experimentally determined for water drops grown on cloud...
A systematic series of condensation coefficient measurements of water have been made using the Unive...
The transfer of gas phase species to aerosols depends critically on the condensation (or sticking) c...
The continuous-flow streamwise thermal-gradient cloud condensation nuclei counter (CFSTGC) is a comm...
The condensation coefficient of water vapor on liquid water and the thermal accommodation coefficien...
The effect of thermal radiation on cloud droplet evolution was investigated both experimentally and ...
A cloud condensation nucleus (CCN) closure experiment is carried out using data from the Chebogue Po...
The determination of cloud formation, water nucleation properties, supersaturation, and droplet grow...
Dropwise condensation of atmospheric water vapor is important in multiple practical engineering appl...
A cloud condensation nuclei counter (CCNC) is used to study the ability of aerosol particles to serv...
The influence of aerosols on cloud properties is an important modulator of the climate system. Tradi...
An expansion cloud chamber was used to measure the homogeneous nucleation rate for water over a wide...
Dropwise condensation of atmospheric water vapor is important in multiple practical engineering appl...
A pulse-expansion wave tube method to determine homogeneous nucleation rates of water droplets has b...
Measurements of cloud condensation nuclei (CCN) concentrations (cm -3) between 0.2 and 1.0% supersat...
Values of condensation coefficient, ß, were experimentally determined for water drops grown on cloud...
A systematic series of condensation coefficient measurements of water have been made using the Unive...
The transfer of gas phase species to aerosols depends critically on the condensation (or sticking) c...
The continuous-flow streamwise thermal-gradient cloud condensation nuclei counter (CFSTGC) is a comm...
The condensation coefficient of water vapor on liquid water and the thermal accommodation coefficien...
The effect of thermal radiation on cloud droplet evolution was investigated both experimentally and ...
A cloud condensation nucleus (CCN) closure experiment is carried out using data from the Chebogue Po...
The determination of cloud formation, water nucleation properties, supersaturation, and droplet grow...
Dropwise condensation of atmospheric water vapor is important in multiple practical engineering appl...
A cloud condensation nuclei counter (CCNC) is used to study the ability of aerosol particles to serv...
The influence of aerosols on cloud properties is an important modulator of the climate system. Tradi...
An expansion cloud chamber was used to measure the homogeneous nucleation rate for water over a wide...
Dropwise condensation of atmospheric water vapor is important in multiple practical engineering appl...
A pulse-expansion wave tube method to determine homogeneous nucleation rates of water droplets has b...
Measurements of cloud condensation nuclei (CCN) concentrations (cm -3) between 0.2 and 1.0% supersat...