An Overview of Lightning Locating Systems: History, Techniques, and Data Uses, With an In-Depth Look at the U.S. NLDN
By Kenneth L. Cummins, M. Murphy. IEEE transactions on electromagnetic compatibility (Print), 2009
671 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Electrical and Electronic Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/1383a7810f756a101bd8369169277f5dd71bbae8
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Citations in the corpus
- Overview of Recent Progress in Lightning Research and Lightning Protection (2009, methodology): “Shao and Jacobson [92] considered both ground and ionosphere-reflected waves produced by lightning return strokes at distances from 200 to 1500 km.”
- Long‐range lightning geolocation using a VLF radio atmospheric waveform bank (2010, methodology): “Since only ground discharges reported by the NLDN are included here, and all low‐current ( 15 kA [Cummins and Murphy, 2009]) positive‐polarity events are labeled as cloud discharges, 14 of 19 there are no low positive peak current events from NLDN. Figure 12a (bottom) shows the percentage of NLDN…”
- Highly intense lightning over the oceans: Estimated peak currents from global GLD360 observations (2013, methodology): “This relationship has been used in many operational applications to estimate the peak current in individual return strokes [Cummins et al., 1998b; Cummins and Murphy, 2009].”
- Rapid Intensification of a Sheared Tropical Storm (2010, background): “Consistent with the findings of Biagi et al. (2007; see Cummins and Murphy 2009), all positive cloud-to-ground flashes with peak current below 10 kA and half the flashes between 10 and 20 kA were removed, because these are likely to represent intracloud flashes.”