THUNDERSTORM T0106 Date: Saturday 27th May 2017
Time:
01:00 Local Location:
Exeter, Devon UK. Path: Few miles west, about 20 miles for Dartmoor cell, and
developing cells overhead
Synoptics:
Plume strongly destabilised by upper trough (low out to the
west) Duration: about 35 minutes Type: Large Multicells (MCS) sharing same Anvil Average lightning type: IC Footage Quality: Full HD
This was one of the most significant
lightshows the southwest has seen in recent years. I haven't seen this
frequency of lightning since being in the US. The initial MCS developed off
the coast of Plymouth and swept north and spread in an arc across Cornwall,
Devon, then eventually Dorset, Somerset and into South Wales during
the early hours of the 27th.
Most of the lightning was high-level
intra-cloud, often in call-and-response with other towers, and the
environment was relatively dry enabling clear view of the towers which are
quite often obscured in these continental plume situations. The upper-level
nature of the lightning with low-CG count meant that the thunder was
relatively quiet and ambient. There were a few positive CGs however, one of
which reached 170kA (see scientific paper below). Not only this, but 23
sprites were observed from the UK Meteor Network. Plymouth saw nearly
continuous 1-4 second discharge rates, mostly up in the cloud with the odd
ground strike, and occasionally less than 0.5s discharge rates (gleaned from
Youtube footage).
[Click to enlarge] CG flash rate by
polarity (blue stacked bar for -CG, red stacked bar for +CG), +CG proportion
(black dotted line) and 5-min average peak current of +CG (red dashed line).
The black circles correspond to the time of observed sprites. Source:
Paper
from Uni of Bath & Met Office,
studying this storm's lightning and sprite activity (Atmospheric Research
Vol 249 (2021) #105357).
Here in Exeter, I arrived late to the
scene just in time for overhead passage. I shot video looking west-northwest
where the bulk of the MCS was developing. In the video, it looks time-lapsed,
but it isn't (apart from the montage at the
beginning). Mature cells weren't quite overhead, but were developing with
some early tower flashes and sparse drops of large rain. The lightning
remained mostly upper-level, often in "call and response" between different
towers, almost giving the impression there was intelligent life up there and
casual chatter.
Environmental conditions were quite unusual for southwest England, yet
perfect for severe elevated storm development. However, these "severe"
environmental conditions were not immediately obvious in model data. It all looked very good in terms
of upper-forcing (very strong cold upper trough), a mid-level jet was
present, feeding pre-heated well-mixed air from a prior cloudless warm day
across France, and a reasonable (but not excessive) amount of CAPE. But
something else was leading to high lightning rates.
There was no Saharan dust present either,
where Saharan dust is thought to enhance lightning rates through giving more
cloud condensation nuclei to the atmosphere and thus offering more ice
particles to charge. One environmental aspect that may have been favourable
was the low vertical wind shear through the column. Normally this would not
be a favourable severe storm condition and can kill cells as they form, but
as the forcing was so strong below and seemingly independent of
downdraughts, the continual pumping of mass into the core anvil aloft perhaps
allowed for very efficient dipole charging.