On 2 stepped leaders in negative cloud-to-ground lightning

Autor(es)

Campos, Leandro Z. S. ^[1] ; Saba, Marcelo M. F. ^[1] ; Krider, E. Philip ^[2]

Afiliação do(s) autor(es)

^[1] INPE Natl Inst Space Res, Sao Paulo - Brazil

^[2] Univ Arizona, Inst Atmospher Phys, Tucson, AZ 85721 - USA

• Tipo de documento: Artigo Científico
• Fonte: JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES; v. 119, n. 11, p. 6749-6767, JUN 16 2014.
• Citações Web of Science: 1

Resumo

In their seminal lightning studies using streak cameras, Schonland et al. (1938) identified four negative stepped leader events that they term 2, a rather rare variant of the type leader, and in it, the second and slower stage of the leader is associated with the appearance of one or more fast dart streamers, which travel rapidly down from the cloud along the previously formed track and cease when they have caught up with the slower leader tip. Seven negative downward leaders that agreed with the description given by Schonland et al. for type 2 were recorded in Tucson, Arizona, USA, and in SAo Jose dos Campos, SAo Paulo, Brazil. All cases were recorded by a high-speed camera operating at 4000 frames per second, and electric field changes were measured for three of them. Their dart streamers had speeds between 106 and 107ms-1, compatible with previous observations of recoil leaders (RLs). Also, during the development of the three cases with correlated electric field changes, it was possible to identify sequences of microsecond-scale pulses preceding the propagation of a dart streamer in the channel. It is proposed that the luminous process that occurs during the development of a type 2 stepped leader is the visible manifestation of one or more RLs that begin inside the cloud and connect to the in-cloud, positive portion of the bipolar, bidirectional leader, and then travel downward to the lower end of the negative stepped leader path. (AU)

• Processo FAPESP: 10/02716-5 - Caracterização das componentes-M e dos líderes de relâmpagos naturais a partir de observações de câmeras de alta resolução temporal e medidas de campo elétrico atmosférico
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