摘要
Intracloud (IC) lightning flashes have been simulated in fine resolution (12.5 m) by using a bidirectional stochastic lightning parameterization scheme within 2-dimensional domain. The simu-lated results show that the IC flashes have a bilevel channel structure and the altitudes of the hori-zontal channels are at the same heights of potential wells, which are supported by the previous VHF source observations and balloon soundings of electric field profile in the thundercloud. Further con-clusions are: (1) After an IC flash is initiated near the boundary between positve and nagetive charge zone, the negative (or positive) leader tends to propagate into the positive (or negative) charge zone. Both types of positive and negative IC flashes have been reproduced and their polarity depends on the up and down disposition of the positive and negative charge regions. (2) The extension range of leaders is correlative with the cloud charge distribution. The leader is possible to extend through the inverted charge region all over where it is extending, but keeps away from the isolated charge area of the same polarity. (3) The channel structures also depend on the electric potential distributions in the thundercloud. Before propagating into the central area of potential wells, the leader tends to extend along the direction with the maximum of potential gradient. Once extending away from the center of potential wells, the leader tends to extend along the direction with the slowest potential change. (4) The IC flash channels have the fractal feature with fractal dimension 1.45 before leaders pass through the central area of charge regions. The exponent decreases rapidly once leaders extend into the low-density charge regions. (5) The induced charges of opposite polarity are deposited in the leader channels within preexisting positive and negative charge regions during IC flash discharges. This causes a new and complicated charge distribution in the thundercloud, and the potential extremum drops from 200 to 20 Mv when the IC flash terminates.
Intracloud (IC) lightning flashes have been simulated in fine resolution(12.5 m) by using a bidirectional stochastic lightning parameterization scheme within 2-dimensionaldomain. The simulated results show that the IC flashes have a bilevel channel structure and thealtitudes of the horizontal channels are at the same heights of potential wells, which are supportedby the previous VHF source observations and balloon soundings of electric field profile in thethundercloud. Further conclusions are: (1) After an IC flash is initiated near the boundary betweenpositve and nagetive charge zone, the negative (or positive) leader tends to propagate into thepositive (or negative) charge zone. Both types of positive and negative IC flashes have beenreproduced and their polarity depends on the up and down disposition of the positive and negativecharge regions. (2) The extension range of leaders is correlative with the cloud chargedistribution. The leader is possible to extend through the inverted charge region all over where itis extending, but keeps away from the isolated charge area of the same polarity. (3) The channelstructures also depend on the electric potential distributions in the thundercloud. Beforepropagating into the central area of potential wells, the leader tends to extend along the directionwith the maximum of potential gradient. Once extending away from the center of potential wells, theleader tends to extend along the direction with the slowest potential change. (4) The IC flashchannels have the fractal feature with fractal dimension 1.45 before leaders pass through thecentral area of charge regions. The exponent decreases rapidly once leaders extend into thelow-density charge regions. (5) The induced charges of opposite polarity are deposited in the leaderchannels within preexisting positive and negative charge regions during IC flash discharges. Thiscauses a new and complicated charge distribution in the thundercloud, and the potential extremumdrops from 200 to 20 Mv when the IC flash terminates.
基金
supported by the National Natural Science Foundation of China(Grant Nos.40205002 and 40475004).
