WWLL Network Global Lightning Locations

 

WWLLN
World Wide Lightning Location Network (wwlln.net)
SYSTEM MESSAGE: Have you tried our Google Earth overlays? Try the one offered by our high speed data distribution partner GuiWeather (and parent WDT) which includes a sample from the last 30 minutes - start with the tab at the top, or zoom in a little with our own 1-hour overlay distribution at WWLLN 1-hour or play them together! RHH

Contact Prof. Holzworth at bobholz@washington.edu , Director of WWLLN, with any questions you may have.
Users of these pages, please click to let us know of your use and suggestions. (RHH )

Americas Lightning
Americas Lightning
Americas Lightning
Americas Lightning
- click on image to get a bigger version -
(Notes: cloud data thanks to National Weather Service/Aviation Weather Center; blue overlay dots are WWLLN Lightning; Red circles are WWLLN receivers; Red line is the terminator)

University of Washington in Seattle operating a network of lightning location sensors at VLF (3-30 kHz). Most ground-based observations in the VLF band are dominated by impulsive signals from lightning discharges called “sferics”. Significant radiated electromagnetic power exists from a few hertz to several hundred megahertz, with the bulk of the energy radiated at VLF.

With our network of sferic sensors we are producing regular maps of lightning activity over the entire Earth. Our map showing the entire world uses coloured spots to indicate lightning strokes (red stars inside an open circle are active WWLLN lightning sensor locations).  Click on the map to expand.

WWLLN Global Map
WWLLN World map

WWLLN Average Density 1deg x 1deg
WWLLN Average Density

Prof Robert Holzworth of the University of Washington produced these data with the cooperation of the universities and institutes which host the stations as listed below. The concept of the toga - time of group arrival - used in the location of lightning was published in a paper (see Publications link below) (University of Otago) ( ).

Wideband VLF spectrograms below show lightning-generated sferics (vertical lines) from our lightning sensors and narrowband signals (horizontal lines) from VLF transmitters. Each spectrogram spans 15s in time (horizontal axis) and 24kHz in frequency (vertical axis) All start at precisely the same time at exactly 0, 10, 20, ... min past each hour. Click on any thumbnail below to expand it to full size (or click on its caption to open it on a new page).

Dunedin spectro
Dunedin

Darwin spectro
Darwin

Brisbane spectro
Brisbane

Perth spectro
Perth

Singapore spectro
Singapore

Osaka spectro
Ōsaka

Moscow spectro
Moscow

Budapest spectro
Budapest

Seattle spectro
Seattle

MIT spectro
Boston

Durban spectro
Durban

São Paulo spectro
São Paulo

Suva spectro
Suva

Los Alamos spectro
Los Alamos

Ascension spectro
Ascension

Mexico spectro
Mexico

Tahiti spectro
Tahiti

Tel Aviv spectro
Tel Aviv

Sheffield spectro
Sheffield

Lisbon spectro
Lisbon

Huancayo Peru spectro
Huancayo

PuertoRico spectro
Puerto Rico

Sodankyla spectro
Sodankyla

Honolulu spectro
Honolulu

Cordoba spectro
Cordoba

Rothera spectro
Rothera

Lanzhou spectro
Lanzhou

Kingston spectro
Kingston

 

CostaRica spectro
CostaRica

Davis spectro
Davis

Boulder spectro
Boulder

UCLA spectro
UCLA


We currently have over 25 sensors logging sferic activity in the VLF band, listed below in the order of their establishment:

Dunedin

University of Otago/Te Whare Wānanga o Otāgo (New Zealand)

Darwin

Charles Darwin University (Australia)

Brisbane

Griffith University, Brisbane

Perth

Murdoch University, Perth

Singapore

National University of Singapore

Ōsaka

Ōsaka University

Moscow

Institute of Terrestrial Magnetism, Ionosphere and Radiowave Propagation (ISMIRAN)

Budapest

Eotvos Lorand University

Seattle

University of Washington

Boston

Massachusetts Institute of Technology

Durban

University of KwaZulu-Natal (South Africa)

Sao Paulo

INPE (Brazilian National Institute for Space Research)

Suva

University of the South Pacific (Fiji)

Los Alamos

Los Alamos National Laboratory

Mexico

Universidad Nacional Autonoma de Mexico

Tahiti

Universite de la Polynesie Francaise

Tel Aviv

Tel Aviv University

Sheffield

University of Sheffield

Lisbon

Portugal Meteorological Institute

Trivandrum

Centre for Earth Science Studies (India)

Huancayo

Instituto Geofisico del Peru

Puerto Rico

University of Puerto Rico, Mayaguez

Cordoba

Universidad Nacional de Cordoba (Argentina)

Finland

Sodankylä Geophysical Observatorya, Sodankylä, Finland

Honolulu

University of Hawaii at Manoa

Rothera

British Antarctic Survey

Lanzhou

Cold and Arid Regions Environmental and Engineering Research Insitute, Chinese Academy of Sciences

Ascension Is.

British Geological Survey and BAS

Kingston and Davis 

Australian Antarctic Division 

Hermanus 

Hermanus Magnetic Observatory and University of KwaZulu-Natal (South Africa)

Boulder 

USGS/Magnetic Observatories (USA)

UCLA 

Dept. of Atmospheric and Oceanic Sciences (USA)

Costa Rica 

Center for Geophysical Research (CIGEFI), University of Costa Rica (Costa Rica)

 

 

 


How it works

We welcome offers of hosting a new WWLLN sensor to add to the list above. All hosts receive all the world-wide data for their own research on monthly CDs. In return, each host provides the computer and meets any local expenses like power, Internet, and maintenance.  However, do not think that a sensor on your own campus is going to give you lightning location data on its own. Only the whole network does that.

Each lightning stroke location requires the time of group arrival (TOGA) from a least 4 WWLLN sensors. These sensors may be several thousand km distant from the stroke. In fact, there is some evidence to suggest that the sensors close to the lightning stroke are unhelpful. The geographical  arrangement  of the sensors is important: a lightning stroke which is enclosed by sensors is much more accurately located than one which is not so enclosed. Clearly a uniform spacing of sensors around the Earth is the ideal. Since the Earth is round, there are no edges: every lightning stroke is surrounded by sensors, but not necessarily by the sensors which sense it. Currently (2004) only about 50% of strokes detected  by one sensor are detected by 4 or more. These strokes are presumably the stronger ones.

To cover the whole world by sensors spaced uniformly about 1000 km apart would require roughly 500 sensors. If spaced 3000 km apart, we would need “only” around 50 sensors. We already have about half this number: mainly in developed countries but not enough in less-developed countries, many of which are in the tropics where lightning is most prevalent.


Direct Weather comparison

WWLLN map with cloud overlay

 

WWLLN map with superimposed cloud viewed by satellite (updated periodically)
(also see other views Americas or Europe/Africa )
(Thanks to National Weather Service/Aviation Weather Center for images of cloud cover).

 

More information

 

More information on the World Wide  Lightning Location network (WWLLN) is available from our publication list


WWLLN Data available
WWLLN Monthly CDs containing all stroke locations over the whole world for 1 month. These are mailed to subscribers within 5 days after the end of each month. Back-issues are available as far back as August 2003. Our site hosts receive a free subscription.

WWLLN Data Files by Internet for recent lightning events (in the last six weeks) are available on subscription for any specified geographical area and time window. We can tailor this service to your data requirements: weekly, daily, hourly, real-time for example.

Contacts

for new sensor locations or WWLLN data subscriptions and back-issues:
Prof Robert Holzworth, Earth and Space Sciences,
University of Washington

bobholz@washington.edu



Webpage maintained by:
Craig J Rodger (University of Otago)
Robert Holzworth (University of Washington)

Lightning image thanks to photolib.noaa.gov

link to noaa photo library
Web editing:
Bob Holzworth (bobholz@washington.edu)