Laboratory investigation of positive streamer discharges from simulated ice hydrometeors
Positive streamer discharges have been observed from ice crystals grown from the vapour under controlled temperature and air pressure corresponding to the standard atmosphere and also constant air pressure of 850 hPa. Crystals of size comparable to larger precipitation crystals were grown in a vapou...
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Published in | Quarterly journal of the Royal Meteorological Society Vol. 132; no. 615; pp. 263 - 273 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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Chichester, UK
John Wiley & Sons, Ltd
01.01.2006
Wiley |
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Abstract | Positive streamer discharges have been observed from ice crystals grown from the vapour under controlled temperature and air pressure corresponding to the standard atmosphere and also constant air pressure of 850 hPa. Crystals of size comparable to larger precipitation crystals were grown in a vapour diffusion chamber at various temperatures and pressures, and were subject to electric fields using an in situ electrode assembly. Results show that individual positive streamer discharges can occur at temperatures from near freezing down to at least −38°C when subject to electric fields on the order of 500kV m−1, in contrast to previous reports of continuous positive streamer discharges occurring only at temperatures warmer than −18°C for pure ice crystals. These results suggest that positive streamer discharges can occur on frozen precipitation particles at high altitudes in thunderclouds, given a sufficiently strong electric field. Such discharges may be a necessary element of the lightning‐initiation process. Copyright © 2006 Royal Meteorological Society |
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AbstractList | Positive streamer discharges have been observed from ice crystals grown from the vapour under controlled temperature and air pressure corresponding to the standard atmosphere and also constant air pressure of 850 hPa. Crystals of size comparable to larger precipitation crystals were grown in a vapour diffusion chamber at various temperatures and pressures, and were subject to electric fields using an in situ electrode assembly. Results show that individual positive streamer discharges can occur at temperatures from near freezing down to at least −38°C when subject to electric fields on the order of 500kV m−1, in contrast to previous reports of continuous positive streamer discharges occurring only at temperatures warmer than −18°C for pure ice crystals. These results suggest that positive streamer discharges can occur on frozen precipitation particles at high altitudes in thunderclouds, given a sufficiently strong electric field. Such discharges may be a necessary element of the lightning‐initiation process. Copyright © 2006 Royal Meteorological Society Positive streamer discharges have been observed from ice crystals grown from the vapour under controlled temperature and air pressure corresponding to the standard atmosphere and also constant air pressure of 850 hPa. Crystals of size comparable to larger precipitation crystals were grown in a vapour diffusion chamber at various temperatures and pressures, and were subject to electric fields using an in situ electrode assembly. Results show that individual positive streamer discharges can occur at temperatures from near freezing down to at least −38°C when subject to electric fields on the order of 500kV m −1 , in contrast to previous reports of continuous positive streamer discharges occurring only at temperatures warmer than −18°C for pure ice crystals. These results suggest that positive streamer discharges can occur on frozen precipitation particles at high altitudes in thunderclouds, given a sufficiently strong electric field. Such discharges may be a necessary element of the lightning‐initiation process. Copyright © 2006 Royal Meteorological Society Positive streamer discharges have been observed from ice crystals grown from the vapour under controlled temperature and air pressure corresponding to the standard atmosphere and also constant air pressure of 850 hPa. Crystals of size comparable to larger precipitation crystals were grown in a vapour diffusion chamber at various temperatures and pressures, and were subject to electric fields using an in situ electrode assembly. Results show that individual positive streamer discharges can occur at temperatures from near freezing down to at least -38 degree C when subject to electric fields on the order of 500 kV m super(-1), in contrast to previous reports of continuous positive streamer discharges occurring only at temperatures warmer than -18 degree C for pure ice crystals. These results suggest that positive streamer discharges can occur on frozen precipitation particles at high altitudes in thunderclouds, given a sufficiently strong electric field. Such discharges may be a necessary element of the lightning-initiation process. |
Author | Petersen, Danyal Beasley, William H. Hallett, John Bailey, Matthew |
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Keywords | Laboratory study tracers Temperature effect Diffusion chamber Cloud discharge low temperature Thunderstorm troposphere Electric discharge Ice crystals Streamer Thundercloud Lightning Electrical corona Electric field Ice crystal Lightning initiation Corona effect Discharge breakdown Atmospheric electricity Hydrometeor |
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References | 2004; 43 1971; 76 2004; 61 1976; 47 2002; 41 2002; 62 1969; 74 1991; 96 1976; 81 2002; 128 1999; 56 1966; 71 1994; 33 1972 1974a 1974b; 50 100 52 1995; 100 1974; 100 1999 e_1_2_1_7_1 e_1_2_1_8_1 e_1_2_1_5_1 e_1_2_1_6_1 e_1_2_1_12_1 e_1_2_1_4_1 e_1_2_1_13_1 e_1_2_1_10_1 e_1_2_1_2_1 e_1_2_1_11_1 e_1_2_1_16_1 e_1_2_1_17_1 e_1_2_1_14_1 e_1_2_1_15_1 e_1_2_1_8_2 e_1_2_1_9_1 e_1_2_1_18_1 (e_1_2_1_3_1) 2004; 61 e_1_2_1_8_3 |
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SubjectTerms | Atmospheric electricity Earth, ocean, space Electric field Electrical corona Exact sciences and technology External geophysics Ice crystal Lightning initiation Meteorology |
Title | Laboratory investigation of positive streamer discharges from simulated ice hydrometeors |
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