scholarly journals Simulation of leader speeds at gigantic jet altitudes

2012 ◽  
Vol 39 (13) ◽  
pp. n/a-n/a ◽  
Author(s):  
Caitano L. da Silva ◽  
Victor P. Pasko
Keyword(s):  
2012 ◽  
Vol 57 (36) ◽  
pp. 4791-4800 ◽  
Author(s):  
Jing Yang ◽  
GuiLi Feng
Keyword(s):  

Eos ◽  
2011 ◽  
Vol 92 (31) ◽  
pp. 264-264
Author(s):  
Colin Schultz
Keyword(s):  

2011 ◽  
Vol 116 (A12) ◽  
pp. n/a-n/a ◽  
Author(s):  
T. Neubert ◽  
O. Chanrion ◽  
E. Arnone ◽  
F. Zanotti ◽  
S. Cummer ◽  
...  
Keyword(s):  

2009 ◽  
Vol 2 (9) ◽  
pp. 617-620 ◽  
Author(s):  
Steven A. Cummer ◽  
Jingbo Li ◽  
Feng Han ◽  
Gaopeng Lu ◽  
Nicolas Jaugey ◽  
...  
Keyword(s):  

2007 ◽  
Vol 112 (D20) ◽  
Author(s):  
Oscar A. van der Velde ◽  
Walter A. Lyons ◽  
Thomas E. Nelson ◽  
Steven A. Cummer ◽  
Jingbo Li ◽  
...  
Keyword(s):  

2020 ◽  
Author(s):  
Jing Yang

<p>At about 22:43:30 BJT (Beijing Time = UTC + 8) on 13 August 2016, two amateur astronomers in Shikengkong, Guangdong province, and Jiahe County, Hunan province, respectively, fortunately captured a gigantic jet (GJ) event simultaneously and the GJ exact location could be triangulated. The parent thunderstorm was in a very humid environment [Precipitable Water (PWAT) in excess of 60 mm], featuring high convective available potential energy (CAPE) and weak 0-6 km vertical wind shear. The GJ occurred in the region with the coldest cloud top brightness temperature of −64 °C, suggesting the GJ was associated with strong vertical development of the thunderstorm. Vertical cross sections of radar reflectivity also show that the GJ occurred near the thunderstorm strong convection region as indicated by the results that a region of 25 dBZ (and 35 dBZ) in excess of the local tropopause (overshooting top in the parent thunderstorm) during a time window containing the GJ. The negative cloud-to-ground flashes dominated during the thunderstorm evolution. Three positive narrow bipolar events (NBEs) were detected within 30s before and after the GJ. It indicates that the NBEs were distributed between 11 and 13 km and occurred in the upper and middle layers of thunderstorm with radar reflectivity of 30-35 dBZ.</p>


2010 ◽  
Vol 115 (D24) ◽  
Author(s):  
Oscar A. van der Velde ◽  
József Bór ◽  
Jingbo Li ◽  
Steven A. Cummer ◽  
Enrico Arnone ◽  
...  

2019 ◽  
Vol 190 ◽  
pp. 6-15 ◽  
Author(s):  
Qijia He ◽  
Jing Yang ◽  
Gaopeng Lu ◽  
Zhixiong Chen ◽  
Yu Wang ◽  
...  

2013 ◽  
Vol 118 (7) ◽  
pp. 2872-2888 ◽  
Author(s):  
Tiffany C. Meyer ◽  
Timothy J. Lang ◽  
Steven A. Rutledge ◽  
Walter A. Lyons ◽  
Steven A. Cummer ◽  
...  
Keyword(s):  

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