NEXSTORM Lightning Page Information & Key.

Our Site

Home
About this station
Station Location

Live Local Weather

Lightning Data
Lightning Data Key

Current Conditions
Daily Highs & Lows
Monthly Highs/Lows
This Years Highs/Lows
History Plots - Week

Archives

This Year
Climatological Summary

Weather Photographs

Weather Images
Burton on Trent - Floods
Gust Cloud & Data
Lightning 26/07/2006
Lightning 12/08/2004
Lightning Images
Shelf Cloud & Data
Sun Pillar
Tornado - 23/08/2004

Space Photographs

Comet Machholz
Moon Images
Sun Images
Nebula Images

Useful Stuff

Storm Chasing
Aurora
Lightning Safety
Photographing Lightning
Storms
Winds

Miscellaneous

Contact

 

 

www.ukspeedtraps.co.uk the UK SpeedTrap Guide

 

Lightning is a giant electrical spark and is caused by the separation of electrical charge in a thunderstorm. The mechanism of charge separation is still poorly understood but there now seems little doubt that ice particle collisions are involved and the conditions favourable to ice particle collisions are strong updrafts which invigorate a thunderstorm's ice factory. Charge separation by particle collisions occurs until the voltage difference in the cloud reaches 10 to 100 mega volts and the local electric field reaches several hundred kilovolts per meter. The latter field is the approximate dielectric strength of the thundercloud medium and its attainment is required to initiate lionization, the initial stage of the large spark that is lightning.

Storm Detection information.

All kinds of lightning (cloud-to-cloud, cloud-to-ground, positive, and negative strokes) are detected by my Boltek detector and with the use of Nexstorm™ to perform the calculations this information gets plotted on a map.. Additionally, two special stroke types, the compact intercloud discharge and the leader are detected from nearby storms as well.

How far away can it detect lightning depends on the intensity of the storm and the kind of terrain between my detector and the storm. Also, I get better "reception" at night. Stronger storms can be detected further away and flat terrain between me and the storm gives me a better chance of "seeing" the storm. Generally, storms within 400 miles will be detected easily. Intense storms have been detected over 1000 miles away.

When the Lightning Detector detects lightning stokes it may take a while to get the position correct, this is due to it recalculating each time. The more strokes the better the position. Some storms will be plotted in the wrong position. The best way to use this data is to look at other sites also plotting the information and average out the data. I will be working with some other users of Boltek units to see if we can produce better storm data and in the future combine the data on to this site and mirror on other sites.

The information is provided for general interest.
It cannot be used for the protection of life or property.

Cloud to ground lightning

Cloud-to-ground lightning is the most spectacular lightning. It is the lightning bolt we see reaching from the sky to the ground forming a bright, usually forked bolt of light. The ground is the most conductive object that will release the most energy. This form usually occurs from the base of a negatively charged cloud. Sometimes there is a rarer form that happens from the the positive charge in the top of the cloud to the negative charge on the ground known as a positive flash. Only about 20 percent of all lightning reaches the ground. Over the entire Earth there are over 100 strikes every second.

Cloud-to-ground lightning is the most damaging and dangerous form of lightning. The great majority of ground flashes are negative, but the most powerful and most dangerous are the positive ground flashes that can also produce sprites in the mesosphere. Positive flashes occur in the decaying phases of large thunderstorms and in the very active stages of severe storms. Most cloud-to-ground lightning strikes come from the negatively charged bottom of the cloud traveling to the positively charged ground below.

Some meteorologists believe that positive lightning strikes indicate storms that are more likely to spin out tornadoes.

Intra cloud lightning

The most common type of lightning, called intra cloud lightning, strikes between positive and negative areas in the same cloud. The bolt is not usually visible, but rather appears like a broad flash in the sky.

Intra cloud lightning is far more prevalent than cloud-to-ground lightning, and the mean peak currents in intra cloud lightning tend to be smaller. Intra cloud flashes that leave cloud base and approach ground, but do not reach ground, are called air discharges. Intra cloud lightning that leaves cloud top and heads upwards are sometimes referred to as cloud-to-ionosphere flashes.

In the active stages of severe storms, intra cloud flashes can outnumber ground flashes by 10-100 to one.

Inter cloud lightning

Intra cloud flashes that bridge two thunderstorms are called intercloud flashes. This less common lightning strike occurs between oppositely charged areas of separate clouds. Known as intercloud lightning, the strike passes through clear air and provides a stunning bolt of light. Intercloud lightning poses a particular hazard to airplanes in flight because it passes through the clear air between clouds.


Key to Live Lightning page

+ CG Positive cloud to ground strike
- CG Negative cloud to ground strike
+ IC Positive in cloud or intracloud strike
- IC Negative in cloud or intracloud strike

Its also worth noting that I may clear off strike data during some storms. This is because I am using the system and removing clutter.

The layout, design and content of this web-site are the copyright material of Steven J Warren.
Copyright 2009 All rights reserved.
DESIGN - www.FlyingBunnyStudio.com

NOT FOR PROTECTION OF LIFE OR PROPERTY
The information here is provided for general interest.