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Record #111373:
Charge transfer during individual collisions in ice growing from vapor deposition / Giorgio M. Caranti, Eldo E. Avila, M.A. Ré.
Title: | Charge transfer during individual collisions in ice growing from vapor deposition / Giorgio M. Caranti, Eldo E. Avila, M.A. Ré. |
Author(s): | Caranti, Giorgio M. Avila, Eldo E. Ré, M. A. |
Date: | 1991. |
In: | Journal of Geophysical Research. (1991.), Vol. 96(D8) (1991) |
Abstract: | Study of importance of fragmentation in charging process. When target is colder than environment, charge pulses have mixed signs, but number of positive ones becomes dominant as target temperature decreases. Behaviour is reproduced in collisions with dielectric particles and target in same growth conditions. Reversal in temperature gradient reversed sign of charge transfer. Direct evidence of fragments produced during collisions suggests that they are responsible for measured charge transfer. |
Notes: | Journal of Geophysical Research. Vol. 96(D8) :15, 365-15, 375 (1991). |
Keywords: | 551.5 -- Meteorology. 551.574.3 -- Condensation, ice particles in clouds. 551.515.4 -- Thunderstorms. 551.578.4 -- Ice needles, sleet, falling snow and graupel. 551.594 -- Atmosphere, electrical phenomena. E9 -- Glaciology: meteorology and climatology. |
SPRI record no.: | 111373 |
LDR 01527naa#a2200000#a#4500 001 SPRI-111373 005 20240419085100.0 007 ta 008 240419s1991####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-111373 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aCaranti, Giorgio M. 245 10 ‡aCharge transfer during individual collisions in ice growing from vapor deposition /‡cGiorgio M. Caranti, Eldo E. Avila, M.A. Ré. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 15, 365-15, 375 :‡bdiags. 500 ## ‡aJournal of Geophysical Research. Vol. 96(D8) :15, 365-15, 375 (1991). 520 3# ‡aStudy of importance of fragmentation in charging process. When target is colder than environment, charge pulses have mixed signs, but number of positive ones becomes dominant as target temperature decreases. Behaviour is reproduced in collisions with dielectric particles and target in same growth conditions. Reversal in temperature gradient reversed sign of charge transfer. Direct evidence of fragments produced during collisions suggests that they are responsible for measured charge transfer. 650 07 ‡a551.5 -- Meteorology.‡2udc 650 07 ‡a551.574.3 -- Condensation, ice particles in clouds.‡2udc 650 07 ‡a551.515.4 -- Thunderstorms.‡2udc 650 07 ‡a551.578.4 -- Ice needles, sleet, falling snow and graupel.‡2udc 650 07 ‡a551.594 -- Atmosphere, electrical phenomena.‡2udc 650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local 700 1# ‡aAvila, Eldo E. 700 1# ‡aRé, M. A. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(D8) (1991) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419