Journal of Geophysical Research Atmospheres · 2014 · 64 citations · 41 references
Natural SciencesEarth SciencesPhysicsAtmospheric ElectricityCloud PhysicsElectromagnetismCloud-to-ground LightningIntra-cloud LightningLightning InitiationLightning PhysicsLightning PropagationThunderstorm ElectricityCloud-to-ground Lightning PropagationInitiationLightning Discharge PhysicsLightning Initiation MechanismsLightning Initiation ModelingPositive Lightning FlashesPotential Field InversionSpace Charge Distribution
Abstract The favorable factors that affect the initiation of intracloud (IC) lightning and cloud‐to‐ground (CG) flashes are investigated by using a fine resolution two‐dimensional lightning model. Simulation results indicate that potential at initiation point is a key to decide whether downward leader reaches ground. The absolute values of initiation potential of CG flashes are greater than 30 MV, while the absolute values of initiation potential of IC lightning are basically less than 30 MV. Since potential field is determined by space charge distributions, polarities and types of lightning discharges are also dependent on relative locations and magnitudes of positive and negative charge zones near initiation points. In general, dipoles (positive charge above negative) initiate normal IC lightning and positive CG flashes and inverted dipoles are associated with inverted IC lightning and negative CG flashes. The magnitude of upper charge near initiation point is generally larger than that of lower charge when CG flashes occur, and the two are comparable when IC lightning occur. For CG flashes, the magnitude of lower charge near initiation points should be enough for initiation breakdown, but not so strong that the lower potential well prevents propagation to ground. In addition, CG flashes are initiated within various special charge distributions, only if the reference potentials at initiation point are far away from 0 MV.
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The tripole structure of thunderstorms
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