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Date: 08-05-1998 to 09-05-1998
Time: 23:55 - 00:48 BST
Location:
Macclesfield, Cheshire UK
Storm Stage: Mature
Path / Movement: Overhead / NW
Footage Quality:
Hi-8
This was the first substantial overhead thunderstorm for 1998 for
Macclesfield, and it was
dramatic in it’s fury too. It was fairly large, close-by, and we had clear displays of
blue C-C in the night-sky after the clock struck midnight, one of which gave
a thunder loud enough set car alarms off and buffet the windows.
It
was a very humid day with a warm-sector airmass feeding up from Spain and France. London
reached its highest temperature of the year so far at 25°C. The showers were
being produced by a mini area of low pressure with a showery trough
positioned in the south of the country.
The whole system was heading north-westwards and on the precipitation radar
on the BBC TV weather forecast there was an area of speckled showers (light to moderate) over
the Midlands heading northwards. Originally I thought they would either
dissipate or just pass over lightly and unnoticed, but I prepared myself
just in case anything developed. The next forecast with a radar image wasn't
for a few hours so I had to stay alert.
As midnight was drawing in, I hung out of the window to smell the
warm and humid spring air of the night, and I thought that it was a perfect
atmosphere for a night-time storm. As I thought that a faint distant flash
occurred in the
corner of my left eye, so I prepared the camera. As it drew in closer, I started
to hear some distant thunder with the lightning flashes, which meant it was
within a good 10-20 mile thunder-audibility range. I started to film
pointing towards the west based on the flashes I saw. After a few more
discharges the lightning was starting to
get brighter and closer and it started raining. It was then I realised the
storm must have been approaching from the southwest.
I had told myself,
before the storm came, that if an overhead storm did eventually come today then
aim the camera up at a higher angle into the sky (than I usually did) to
capture any overhead I-C or C-C lightning. In 1997 I used to aim the camera so the
ground was visible in order to capture the full arc of C-G strikes, and as a consequence
I was missing what was going on overhead. So I aimed the camera upward and it
was about to pay
off. Eventually the rain fell harder as the storm passed directly overhead, giving
a total of four
excellent close-up displays of C-C, I-C and a few other distant C-Cs and
flashes. I wouldn’t have got these brilliant new shots if I hadn’t have
aimed the camera at a higher angle.

The first C-C took me completely by surprise. I hadn't realised the lightning
hotspot of the storm-cell had crept directly overhead until I was blinded by two incredibly bright C-Cs streaks
across the sky. I had to blink afterwards it was that bright as I could
still see the outline of the lightning burnt into my retinas, and if that wasn’t
enough I was deafened as well. Precisely eight seconds after the discharge the most
phenomenal thunder I’ve
heard
crashed across the landscape setting off car alarms and buffeting the windows
(more about this later). The following close-by C-Cs weren’t as energetic as
the initial. This I can justify because the
second C-C was exactly the same distance away judging off the thunder, maybe a fifth of a mile
closer, and the thunder wasn’t even half as loud. This shows how
lightning can vary in electrical properties depending on the
magnitude and environmental conditions of the discharge. Most of the remaining lightning
discharges were seen as C-Cs with branches and feelers, somewhat extremely photogenic and
beautiful.
Here are some detailed statistics of the initial loud thunder at the
beginning. It
took 8 seconds for the first thunder-waves to travel from the lightning to
where I was, which was equivalent to approximately 1.6 miles away (2.67km).
This is a fair distance for a thunder of this magnitude. Unusually high-amp lightning,
possibly C-C in conjunction with an unseen P-F (positive flash) occurrence,
was most likely the cause of this. The thunder was about 30 seconds
in duration suggesting that it may have been of upper-anvil origins with
along-channel.
Edit: I am writing this
current paragraph December 2007 and the archive is currently up to T0072.
Sixty-one thunderstorms
later and I have yet to witness anything to match the ferocity of the
thunder in this storm, including discharges occurring at a quarter of
the distance as this one. This single discharge together with the
spectacular C-C shows has earned T0011 "Storm of the Year" by a country
mile. Check out the video below.
CLICK BELOW FOR VIDEO OF IMMENSE DISCHARGE (Youtube)
http://www.youtube.com/watch?v=s_PzUs1wqq0
ANALYSIS OF EXTRAORDINARY THUNDER
|
Time (seconds) |
Length (seconds) |
Description |
|
0.0 |
1.8 |
Build Up |
|
1.8 |
2.5 |
1st set of bangs - 5
Loud Bangs |
|
4.3 |
0.5 |
Main Rumble and
Aftershock Rumbles |
|
4.8 |
2.0 |
2nd set of bangs - 3
Longer Bangs |
|
6.8 |
23.2 |
Aftershock Rumble
and Echoes |
|
30.0 |
|
End |
WETTERZENTRALE SPHERICS
(CREDITS)
EUROPE 24-hour 8th May LIGHTNING SPHERIC LOCATION
EUROPE 24-hour 9th May LIGHTNING SPHERIC LOCATION
DUNDEE SATELLITE IMAGES
(CREDITS)
VISIBLE 08.05.1998 16:46
INFRARED 08.05.1998 16:46
COLOUR 08.05.1998 16:46
INFRARED 09.05.1998 03:35
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