science & techanalysisEos

Decoding the Origins of Lightning’s Violent Currents

the gist

The return stroke is the surge of current that races upward through a lightning channel once a leader from the cloud connects to the ground. It carries tens of thousands of amperes at a sizable fraction of the speed of light, producing the flash, the thunder and the radio pulse that detection networks use to locate strikes. A review by researchers at New Mexico Tech shows that the Telegrapher's Equations, the same framework used for signals on power cables, can explain its shape. The current rises quickly when the leader connects and decays more slowly because of the channel's resistance. The same model explains why the wave travels slower than light, weakens with height and spreads out as it climbs.

how it works

The lightning channel is modelled as a long conductor with resistance, inductance and capacitance spread along its length. Charge stored in the sheath around the core is neutralised as the wave moves, and the balance between these effects sets the current's rise, decay and speed.

so what

Return strokes cause much of lightning's damage, including billions of dollars a year to power and communication lines and many wildfire ignitions. They are also the atmosphere's main natural source of nitrogen oxides, so understanding them matters for both safety and atmospheric chemistry.

Eos (AGU) · CC BY-NC-ND 3.0

Illustrative photo · Mathias Krumbholz, CC BY-SA 3.0, via Wikimedia Commons