WWLLN (World Wide Lightning Location Network) By Prof. Robert Holzworth, Director of WWLLN, University of Washington.

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Presentation transcript:

WWLLN (World Wide Lightning Location Network) By Prof. Robert Holzworth, Director of WWLLN, University of Washington

WWLLN statistics 55 stations operating (60 actually delivered) million strokes/month Detection Efficiency Estimates:  >95% of lightning producing thunderstorms  ~11 to 20% of global total strokes  >30% of strokes over 60 kA

2009

Detection Efficiency compared to NLDN * Study done by independent researcher at UCLA (2010)

How does it work? TOGA Fourier Synthesis: Dispersion Case Problem Detecting Global Lightning: The Sferic from the lightning strike has many frequencies and these waves travel at frequency dependent speeds so all 100 waves we use in our analysis don’t come into phase.

TOGA Provides Better Location and Timing Accuracy than Trigger Time Sferic detected with TOGA marked (blue) and Trigger Time marked green Using TOGA instead of trigger time allows timing to <30 μs and location accuracy to 5-10 km anywhere in the world. Trigger time Time of Group Arrival (TOGA)

Each WWLLN Station detects lightning out to 12,000 km at night and 8,000 km during the day

Energy/Stroke now being produced APP files now have power per stroke information. Being produced daily. Historical power data back to April Regular production planned by end of year

Figure 6. Hutchins et al, 2011 WWLLN peak current versus NZLDN peak current for three time periods in 2009 using 12,015 matches. 86% of strokes are within range of the unity line (red solid line) with uncertainty taken into account. 97.5% of NZLDN-WWLLN matched strokes shown (others out of range)

WWLLN stimulates New Research Ionospheric Plasma effects –Sprites/Jets/Elve research –Ionospheric EMP –VLF propagation (tweeks determine D-region density) Atmospheric Science –Hurricanes dynamics –African Easterly waves –MJO shown to have strong lightning signal Terrestrial Gamma Flashes Volcano Ash Cloud Lightning See

80-day high-pass filtered 5° latitude × 5° longitude Global Precipitation Climatology Project precipitation (mm day-1) regressed onto time series representing phases 1-4 (top to bottom) of MJO index. Adapted from Virts and Wallace [2010]. Virts, Katrina S., Joel A. Thornton, John M. Wallace, Michael L. Hutchins, Robert H. Holzworth, and Abram R. Jacobson, Daily, seasonal, and intraseasonal relationships between lightning and NO2 over the Maritime Continent, Geophys. Res. Lett., doi: /2011GL (in press), 2011

80-day high-pass filtered cloud fraction (left), lightning (middle), and NO2 (right) regressed onto time series representing MJO phases 1 (top) to 4 (bottom). Regression coefficients are scaled by the annual mean; gray shading indicates areas of low annual mean

Sarychev Redoubt Sarychev

WWLLN Volcano Monitor (see ) WWLLN examines 1,562 volcano caldera every minute to look for lightning within two rings: within 20 km of the caldera, and with a larger ring at 100 km. If new lightning is found in the inner ring, and over the last hour there is MORE lightning in the inner ring, than the outer ring, WWLLN sends an ALERT message to the USGS about the possibility that an eruption is underway. Presently alerts are only sent for Alaskan Volcano Observatory volcanos, but ALL volcanos are monitored every minute. Since turning on the Alert system in Oct 2010, WWLLN has correctly identified three explosive eruptions, giving volcano centers up to 1 hour early warning, compared to available alternative methods of eruption detection and confirmation. Most recent Dec 31, 2010 (Kizimen, Kamchatka) (this is old now)

Future Plans Add Energy per stroke and dynamic detection efficiency to real time processing (for now it is being produced as a daily file, once a day, offline from the regular processing) Calculate a dynamic (realtime) Detection Efficiency Combine raw data from ENTLN with WWLLN to greatly improve the detection efficiency

WTLN waveform

Finding TOGA from Weatherbug waveform

We are Research Driven WWLLN is a consortium of researchers. Our goal is to detect as much of the global lightning as possible with high time and space accuracy. We cannot afford data dropouts. We value redundancy and have removed possible single point failures. We collect the data and we use it in our own research. If it is useful to you, then we’ll be glad to sell it to you, too.