Download or read book Study of Spacetime and Electrical Properties of Artificially Triggered and Natural Lightning Discharge Based on VHF and Electric Field Observations written by Yanchi Shen and published by . This book was released on 2017 with total page 195 pages. Available in PDF, EPUB and Kindle. Book excerpt: The space charge density of L1a increased as the leader developed. The general range of the space charge density of L1a under 680 m high was -3 nC/m3 to 5 nC/m3, with some unipolar pulses (-31 nC/m3 to 72 nC/m3). The space charge density of L1a above 680 m high was very small and ranged from -0.8 nC/m3 to 0.4 nC/m3. These pulses indicate that there were positive charge groups present. The allocations of the pulses of the space charge density were the same as for the bipolar pulses of the background electric field, the pulses of the negative line charge density, and for the big curves of the L1a channel. Therefore, the complexity of environmental electrical conditions can cause distortion of the leader channel. Similar conclusions can be drawn for the L2a channel, except in the smaller range of the space charge density. The range of the space charge density for L2a was from -0.4 nC/m3 to 0.45 nC/m3, with some large pulses ranging from -8 nC/m3 to 8 nC/m3. Due to the limitations of this approach, the ranges of the background electric field and space charge density may not be accurate, but the trends and the pulses further our understanding of the propagation of lightning discharge. Fourth, using a similar approach as for the triggered lightning discharge, we studied the spatial and electrical properties of natural lightning discharge. As we had no optical images of the natural lightning, its channel was rebuilt by the data of the VHF source radiation from the broadband interferometer with a presumed height of the lightning initiation position in the cloud. Based on the approximate channel that was rebuilt, it was found that this discharge was a downward stepped-leader initiated negative cloud-toground discharge with only one leader/return stroke process. The general speed of the leader when it propagated horizontally in the cloud was 0.4 ×106 m/s to 1 ×106 m/s, and when it propagated vertically was about 3.5 ×104 m/s to 1.5 ×105 m/s. The average speed was 7.0 ×10 4 m/s. As it went downward, the leader branched significantly. Additionally, while the leader moved downward, the VHF sources (breakdown processes) within branches around the leader tip frequently showed backward movements (about 400 m) with a speed of about 2 ×106 m/s, which is much faster than the average leader downward speed of 7.0 ×104 m/s. Electrical properties of the leader above 3000 m were also obtained based on a rough leader channel without branches and backward movements. With the development of the leader channel, the leader brought negative charges downward along the leader channel and the changes of the electric field increased. The estimated line charge density showed a trend to increase as the leader propagated downward, ranging from -0.1 mC/m to -1.1 mC/m. The pulses of the leader charge density show that the leader transported plenty of negative charge when it propagated along the leader channel, which may have caused the curves of the leader channel. Lastly, the findings and their scientific merits are summarized and discussed. Through our study of artificially-triggered lightning discharge and natural lightning discharge, we know that while the cases analyzed here are special, they have some common features. The range and the trend of the electrical and spatial properties show the applicability of the approaches and models in my study. The changes of electric field observed on the ground, the space evolution of the lightning leader channel and the propagation speed of the leader channel were closely related to the spatial initial environment of the lightning discharge. Differences in environment can cause different propagated movement of lightning discharge, depending on the results. This means that a different distribution of space charge or a complex environmental electric field profile can lead to a complex leader channel and movement. A stronger background electric field indicates stronger VHF radiation sources, a faster speed of the leader channel, a more complex lightning channel and more charge in the leader channel. In future research, we need to improve the methods of observation, to obtain more detail of the lightning discharge. With high resolution observations and more sophisticated detail for the lightning discharge, additional spatial evolution characteristics and electrical properties of the discharge, such as the charge density of the branches of the leader channel, can be analyzed. The accuracy of the results also will be improved. Lightning discharge with more complicated initial electrical environments also can be studied in the future, using observation and simulation.