They also use a time-of-arrival technique to locate source points in 3 dimensions and time, usually using at least 6 or 7 stations to keep errors lower. LMA systems also detect radio noise, but in the very high frequency (VHF) band around 60 MHz. NSSL is currently building a mobile array in order to provide targeted lightning observations in conjunction with field campaigns. Research LMA's exist in Oklahoma, the Texas Panhandle, northern Alabama, Washington D.C., Kennedy Space Center in Florida, and many other locations. Up to thousands of points can be mapped for an individual lightning flash to reveal its location and the development of its structure. Lightning Mapping Arrays provide three-dimensional mapping of lightning channel segments near the array. What we do: NSSL uses the data collected by the NLDN to learn how storms produce CG flashes and how these flashes relate to other storm hazards. The +CG return stroke, however, more often has a sustained current that can have greater chance of igniting fires. Positive CG (+CG) flashes effectively bring positive charge to ground (or negative charge up) and almost always have only a single return stroke. CG flashes that bring negative charge from the cloud to ground (“negative CG” or “-CG”) can have multiple return strokes, which can sometimes be seen visually as a flickering of the channel to ground. Flashes outside of the network have larger location errors and may not even be detected.Įach system may detect more than one stroke (in-cloud or return) for a single lightning flash. Location accuracy is best when lightning occurs within a network of stations. Radio signals are detected by multiple stations (at least 3) are used to determine the location of the stroke by a time-of-arrival technique. Since there are many other sources of radio noise, the systems have to first identify which bursts are likely to be caused by lightning. CG return strokes usually have larger currents that make stronger signals that are easier to detect. A “stroke” can be a fast current within the cloud, or a “return stroke” in a channel to ground. These two systems work by detecting radio waves (sferics) emitted by fast electric currents (strokes) in lightning channels.

I was interested in the Met Service map because it appears to show both c-g and c-c strikes - and I’m disappointed to hear that it’s only available by subscription.Severe Weather 101 Lightning Detection Lightning Detection NetworksĬurrently, cloud-to-ground (CG) and intra-cloud (IC) lightning flashes are detected and mapped in real-time by two different networks in the United States-the National Lightning Detection Network (NLDN), a system owned and operated by Vaisala Inc, and the Earth Networks Total Lightning Network.

It certainly does not register at least half of the lightning flashes I have observed during storms.

IMO it’s pretty useless - I believe it only records cloud-to-ground strikes and not cloud-to-cloud (or vice versa). I have looked at Blitzortung for years when I’ve been in electrical storms in NZ and several other countries. Thanks - I was aware of all those sites and I believe they all source from Blitzortung. They are all very similar and possibly just aggregated from the same source There is a number of free Live Lightning Trackers for NZ, but the MetService one is via their industry system and then another subscription

Real time lightning tracker