Characterizing the TGF-Lightning Relationship Using ENTLN
Abstract:
Examining all TGFs with strong ENTLN radio associations reveals three distinct timescales of activity. The shortest timescale component includes radio signals within ±200 µs of the TGF. The second component includes radio signals within ±6 ms of the TGF. The third component occurs after the TGFs out to ~800 ms.
Signals in the first component are predominantly the TGFs themselves. The pattern of signals in the second and third components confirms the hypothesis in which IC lightning travels from the upper negative charge layer to the upper positive charge layer, generating a TGF, followed by a flurry of further lightning activity that propagates through both layers. Specifically, the second timescale component consists of vertical strokes, during which TGFs can occur randomly. The third component is the horizontal activity that follows.
