Author : Peter Berdeklis
Publisher :
ISBN 13 :
Total Pages : 0 pages
Book Rating : 4.:/5 (133 download)
Book Synopsis The Ice Crystal-graupel Collision Charging Mechanism of Thunderstorm Electrification by : Peter Berdeklis
Download or read book The Ice Crystal-graupel Collision Charging Mechanism of Thunderstorm Electrification written by Peter Berdeklis and published by . This book was released on 1998 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: The ice crystal-graupel collision charging mechanism, which is considered important in thunderstorm electrification, was studied using a newly developed Triple Interaction Facility. The facility is the first to allow independent control of the solid, liquid and vapor phases of a simulated cloud. The charge transferred to a riming target by collisions with ice crystals was measured over a wide range of cloud conditions. It was found that the charge transfer was a function of the temperature and the effective liquid water content of the cloud. It was also found that the charge transfer to the target was extremely sensitive to the relative humidity at which the ice crystals were grown. Higher relative humidity always promoted stronger negative charging, while lower humidity led to weaker negative or stronger positive charging. The sensitivity of the charge transfer to relative humidity was greatest at temperatures between-13°C and-18°C, with the strongest negative charging observed near-15°C. Within this temperature range the average charge transferred to the target could be varied from +5 fC per ice crystal collision to -25 fC per collision by varying the humidity from ice to water saturation, respectively. In experiments performed at humidities near water saturation and at temperatures near -15°C, charge transfers greater than -60 fC per collision were observed within the first 30 seconds after ice crystals are initiated. It was also found that at high relative humidity the maximum negative charge transferred to the target occurred at a velocity of 5m s-1 and was much weaker at 3, 4 and 6 m s-1. A parameterization of the results is presented for use in numerical thunderstorm models. Analysis of the data indicates that a competition between negative charge transfer between the liquid-like' layers of the colliding ice particles and positive charge transfer due to different dislocation densities can provide a consistent physical model of the effect of relative humidity. It is shown that differences in. the relative humidity can explain quantitatively the discrepancies between the observations of previous investigators. A new conceptual model of thunderstorm electrification is also presented.