THUNDERSTORM T0011 Date: Friday 8th May 1998 Time: 23:55-00:48
BST Location:
Macclesfield, Cheshire UK Path: Overhead
Synoptics: Early continental plume Duration: 53 minutes Type: Mid-level multicell Average lightning type: C-C Average discharge rate: 2 minutes
Footage Quality: VHS
This was the first substantial overhead thunderstorm for 1998 for
Macclesfield, and it was
dramatic in it’s fury. It was fairly large, close-by, and we had clear displays of
blue lightning 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 humid day with a warm-sector continental airmass feeding up from Spain and France. London
reached its highest temperature of the year so far at 25°C. The airmass,
likely with preconditioned instability from Iberia, was destabilising ahead
of an extending upper trough associated with an Atlantic depression.
The system was heading north-westwards and on the precipitation radar
there was an area of speckled showers (light to moderate) over
the Midlands heading northwards. Initially I thought they would either
dissipate or just pass over lightly and unnoticed, but I prepared myself
just in case anything developed. The next radar image I saw wasn't
for a few hours (the days before internet - relying heavily on BBC weather) 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 (traditionally). 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 15-20 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 then told myself,
based on errors I made during 1997, that if an overhead storm did eventually
come today then aim the camera up at a higher angle into the sky and forget
about the horizon (for CGs), so I could to
capture any overhead I-C or C-C lightning. 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 upwards.
The first C-C took me completely by surprise. I hadn't realised this
particular cell was directly overhead (must have matured whilst arriving) 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 quickly deafened as well. Precisely eight seconds after the discharge the most
phenomenal thunder I’ve
ever heard
(still to this date in 2020) 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
a long channel.