Chase July 10: III

2010.07.18

The rest of the pictures of the July 10 Chase…

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Het Kleine Bliksemboek

2009.09.25

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The little lightning book… after a few years of chasing we finally managed to collect enough pictures for the little book. Well, to be honest, the big lightning book is following with a bunch of other weather related books. The book is for sale through blurb or you can buy it directly from us (Peter and me). For friends this could be a lot cheaper since you don’t have to pay any shipment costs. The book is for sale for 14,95 Euro and that’s for the softcover version. Hardcover version is slighly more expensive. More info can be found here


An out-focused chase…

2009.07.27

First chase this year… it felt as the best ever until I watched the pictures… everything during daylight was pretty correct in focus but as soon as light vanished and was replaced by nightly arial electricity I somehow lost my built up experience to make some beginners mistakes of the first order.  Or how to stay with your feet on the ground when all conditions are perfect. But that won’t stop me from writing a little report about this fabulous chase. I still have seen what I’ve seen, the only link missing is the traduction between my eyes seeing lightning and what other people will see on the pictures. I must have a blurry view of the world… Anyway…

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Underneath a short report…

As Peter reported already a few days ahead, the 21 of July would be a good day for a chase. I left around 2.30 PM for Gent. Late as usual,  when I arrived Peter was quite excited. Bart was already there and together they were checking out the latest radar and sat images.

There wasn’t a lot of time left… convection was forming extremely rapidly within matters of half an hour. It was clear that Estofex predictions were quite correct again… (A level 2 was issued for parts of Belgium, the Netherlands and extreme NW-Germany mainly for large hail, severe wind gusts and tornadoes.Benelux, Northern Germany… An elevated mixed layer covering central and southern France will be advected northeastward during the day and should overspread the Benelux and much of Germany during the afternoon hours. Wind shear will be very strong under the southwesterly jet that consists of two separate speed maxima: one should stretch from north-central Spain across France to NE France, whilst the other is located over the Channel region and SE England. A zone of high, 200-300 m2/s2, storm-relative helicity, should move northward along the leading edge of the elevated mixed layer, and values around 200 m2/s2 should also be locally further south across central and southern France. Moreover, 0-3 km shear will be in the 20-25 m/s range, which is strong.

Models are insofar constistent with each other, that they all produce precipitation in the late afternoon and/or evening across the Benelux and NW Germany, and some further east along the warm front as well. But some models produce only little convection. Apparently, the overall forcing for upward motion is not very large. Still there is confidence that significantly more than just one or two storms will develop. Because of the excellent kinematic and thermodynamic parameters, the storms have a significant potential to become severe, and a level 2 is issued as a consequence. The storms will likely include supercells. Storms across the Benelux and northern Germany will be capable of producing large hail and damaging gusts, and also tornadoes. The tornado risk will be largest with those cells that tap most of the helical low-level flow: those that ingest the most backed low-level winds. The storms are expected to continue throughout the evening, and new storms could even develop overnight. However, those will probably be elevated and because of low-level cooling, they will be less likely to produce severe winds or tornadoes.)


The only thing Estofex isn’t doing yet is predicting the place where we need to go to have the best pictures… Anyway, we hit the road quite fast after a check-up in the local gas station. Headed straight away for Vinderhoute where we had a first series of stops. First stop on a bridge… see on the next page for the rest…

A bolt from the blue…

2009.06.13

  Underneath is a picture that wired magazine bought from me to use… and they actually changed the defenition of the word “use”… maybe they should have altered it a little more… i.e. … beyond recognition… but by tomorrow I’ll maybe thinking about it in a different way.  Anyway, blue it is and here’s the link where to find it, maybe it’ll look better on glossy paper…  I kinda feel dual about it, happy to have a picture in a magazine but not happy to see it so altered…

WIRED MAGAZINE: ISSUE 17.06

In the Strike Zone: What Lightning Teaches Us

By Sarah Douglas  05.235.09 | 6:00 PM
START

Lightning comes in more flavors than you can shake a metal rod at—positively or negatively charged, headed up or down, hitting the ground or another cloud. Atmospheric scientists know that ice particles in a thundercloud become slightly charged. Eventually, a negatively charged layer of the storm gets sandwiched between two positives. Electricity arcs among the layers, ionizing the air and making it glow. But experts have yet to understand the bolts’ behavior. Researchers are now tracking the radio waves and x-rays produced by lightning, and they’re even experimenting with synthetic strikes (made with rockets!). Here’s their current thinking.

11 Types of Bolts

1. Gigantic jet

About 80 percent of all storm discharges are intracloud. But if one heads up and hits a weak positive charge in the upper layer, it exits skyward.

2. Bolt from the blue

Gigantic jets can exit the cloud sideways and touch down miles away from the storm that spawned them under a clear blue sky.

3. Spider

These discharges travel up to 60 miles per second over huge distances, moving laterally through horizontal layers.

4. Beaded

Certain segments of the kinked ion channel seem to glow brighter when seen from a particular angle.

5. Forked

When too much negative charge builds up at the end of a bolt, its channel can split apart in midair to form two or more offshoots.

6. Ribbon

Multiple strikes sometimes share the same channel. If the wind blows the channel sideways, the eye perceives a band of light in the microseconds between strokes.

7. Zigzag

As a storm dissipates, air between the cloud and the ground holds pockets of charge. This produces bolts that hop groundward from one pocket to the next.

8. Ball

Grapefruit-sized, glowing spheres of electricity have been reported in the vicinity of thunderstorms. No one knows why.

9. Energetic narrow bipolar

These intracloud flashes are one of the strongest natural source of radio emissions. They last only 10 microseconds.

10. Red sprite

Positively charged cloud-to-ground lightning makes the cloud more negative. That negative field reaches upward above the cloud, where lower air densities mean less energy to produce a discharge—which then glows red.

11. Blue jet

According to one theory, negatively charged cloud-to-ground lightning makes the cloud more positive; the storm pumps the excess positivity skyward in a high-energy burst that makes the ionized air around it glow blue.

 

Photo illustration: John Blackford 
Photograph by Olivier Vandeginste/atmospheres.be

And the original… just some small changes as you can see…




A massive shelfcloud

2008.11.02

Chase started in the neighborhood of Moeskroen. A darkening sky to the South and also towards the  West promising convection. On the way to Brussels we made several stops: Molenbaix and Hoves just along the highway where we had a beautiful sight on the beginning of the forming shelf. Pictures from that day are in the bottom of the page. Pictures and animations from Peter can be found here.

Read more…

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