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 inQuarterly journal of the Royal Meteorological Society Vol. 132; no. 615; pp. 263 - 273
Main Authors Petersen, Danyal, Bailey, Matthew, Hallett, John, Beasley, William H.
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.01.2006
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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
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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  fullname: Hallett, John
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  givenname: William H.
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Issue 615
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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Snippet Positive streamer discharges have been observed from ice crystals grown from the vapour under controlled temperature and air pressure corresponding to the...
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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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