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Eagle Eye

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Posts posted by Eagle Eye

  1.  

    This does appear to be a real video as there's a similar shot from further away of the dead man walking structure of one of the tornadoes with multiple large vortexes. Suggestive that it cold well have been violent. 

    • Like 1
  2. I was supposed to have a forecast out today but unfortunately the person that makes the maps couldn't make one today. Heres my discussion.

    A trough behind an occluded front should bring heavy showers to the south coast. A Theta-E lobe advecting northwards with the trough will allow for channel and south coast showers throughout the afternoon and evening behind a clearing occluded front to the north and east which may also bring the risk of the odd sporadic lightning strike earlier in the day to a lot of the country but the risk is quite low.

     

    This moisture convergence should form widespread clusters of showers, some reaching 7km tall or around 23,000 feet potentially. Given relatively high shearing and 100+ J/KG of 3CAPE in areas, lightning is likely but mostly should be sporadic because of the messy nature of the showers and given similar events, very little could come out of the lightning but if they linger into the evening and scatter, I've seen lightning increase then.

     

    Small chance of a Supercell and potentially a tornado mainly in the SE given the shearing but apart from that, there's really little support for either except low LCL's. Small hail may form but I wouldn't say is likely just given that the MLCAPE is mostly quite weak and mixed in at the warmer lower levels rather than where the temperature is below freezing.

     

    High saturation for a lot of the south also limits lightning but having looked at many soundings, the saturation varies a lot from place to place and some areas have very weak saturation with favourable lightning conditions just miles away from high saturation and unfavourable lightning conditions. It's a very messy setup which makes it a bit more difficult to forecast for specifics.

    xx_model-en-341-0_modswisseu_2024030100_18_4855_240.thumb.png.6f8f8bafa09d53d0296db4451196278b.png

    xx_model-en-341-0_modswisseu_2024030100_18_4855_247.thumb.png.8be24a61c974341407d5524b8df4dcb8.png

    xx_model-en-341-0_modswisseu_2024030100_18_4855_1233.thumb.png.c94ae915eb3e7b239927bf40fdccedec.png

    • Like 6
  3. Reed dominating as usual, already up close and personal with the crazy storms of course. Started off very quickly. Got close to a funnel cloud that was just about touching the ground and as always with Reed it was a "Big time tornado" but definitely a fast start.

    • Like 1
  4. Focus is now on tomorrow

    All modes risks. 

    Conditionally severe tornadic potential I would say based off mode. High 3CAPE and low freezing with a classic C low-level hodograph is looking fairly favourable for severe hail I would say. 

    Along with that, the low LCL's and fairly high DCAPE should convert a lot of that into downwards momentum for severe wind gusts as well. Don't think it's massive and only slightly severe favourable DCAPE but if linear mode can be upgraded to further, that could go hatched but  I think we're too late for that strong of an upgrade. 

    The low LCL's, high vorticity and low-level energy could contribute to tornadic development. This would especially be evident with isolated Supercells away from the clustering currently forecasted. An isolated Supercell taking up the environmental potential could cause a significant tornado but it's very conditional on that isolated Supercell forming in all the mess. 

    hrrr_2024022612_038_42.36--84_86.thumb.png.b9b3f113b9fe908e4ba59f2dc8244457.png

    • Like 2
  5. Another day, another set of circumstances for me missing lighting. First off, first mini-distant storm, had to charge my camera. Second mini-distant storm set camera to 20 second exposures automatically for a burst, 2 seconds after the burst finishes, lightning strikes, a CG, that I saw on my camera as it was on but it had just stopped filming and if there would've been 1 more picture to the burst I would've got the lightning.

    • Like 5
  6. Fun examples of a leading stratiform region from the cold front driven first squall ahead/in line with the low/developing low to it's north tilted SE. 

    Screenshot_20240222_115914.thumb.jpg.5e02682c3fed4223e201f1e6f6647f22.jpg

    Whereas the NE tilted system with a leading stratiform region from a trough behind the low's centre. 

    Screenshot_20240222_114805.thumb.jpg.944bb250e350be946c18a4f1de6c54de.jpg

    Leading stratiform region - Winds flowing back to front. 

    Trailing stratiform region - Winds flowing from front to back. 

    With the pulling towards a low pressure it makes total sense. 

    Let's talk cell motions as well. 

    Following the shearing direction. The majority of the low-level shear should contribute to NE movement, whereas cell motion from a lot of what I see appears to follow the upshearing direction which is SE. 

    Polish_20240222_123814707.thumb.png.0276e91a89cc305844ff36534c069df5.png

    Hence the bottom cell moves SE whereas the system moves NE. Also watch how the cell just to the south of the one I highlighted also moves SE. 

    Polish_20240222_122541475.thumb.jpg.7e2545163e2acc7f4528b4310dd68d26.jpg

    Screenshot_20240222_122454.thumb.jpg.97b3cf5d2b88e6b920654767a83a56a8.jpg

    Storm movement is still NE here with the shearing direction NE but cell motion should also be NE as the upshear is slightly NE of surface shear. 

    Polish_20240222_123519638.thumb.png.428615b9961afa9ef7aa9ec839335bbc.png

    There we go, yes they're all moving NE. There's still replacement cycles though and especially away from France as we've seem it can easily get messier over the channel. 

    Screenshot_20240222_122954.thumb.jpg.cf8e5370983adaf963ed99d3d8d5c78e.jpg

    Screenshot_20240222_123010.thumb.jpg.341585aaed25d5a25fbb54c9492e0b8f.jpg

    • Like 2
    • Insightful 2
  7. Great example of a cycling mini-squall line today. These occur with interactions between the cold pool strength and low-level shear strength. 

    1) Tight squall line with weaker trailing stratiform behind it, loses shape as the stratiform region is stronger.

    20240220_164434.thumb.jpg.e634529a6d1a1ffe9e09d701a674e190.jpg

    2) Development of cell into the system temporarily outbalances the cold pool and the frontal lobe of the mini-squall tightens. Except for where it disconnects further north with less momentum and shearing effects. 

    20240220_164438.thumb.jpg.1cc292f52e5f13fefa1c4ab975ca81f8.jpg

    3) Once the new cell cycles into the system, the cold pool re-strengthens and timilts the updrafts back for most of the frontal lobe of convection leading to a loss in the uniform linear mode. Squall line loses shape. 

    20240220_164443.thumb.jpg.4bfd97996be333ca6ffc823d9be4d873.jpg

    4) As this loses energy, the stratiform region becomes the dominant force and it loses all shape. This is where the mini-squall is unlikely to reform properly till it re-encounters energy. 

    Screenshot_20240220_170254.thumb.jpg.17cf95d8f3b17c4f224f2c6c5afa4176.jpg

    • Like 1
    • Insightful 5
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