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Nick B

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Posts posted by Nick B

  1. 42 minutes ago, IDO said:

    Big differences in the outcome between ICON and GFS, even at D4, with only subtle variations in the micro-scale (T108):

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    ICON has us in a cold trough and GFS within a high. With so many differences so early, next week is a difficult forecast. However, the macro pattern may still end similarly.

    Indeed, but for me a notable point of interest this morning is in fact the quite unusual similarity in overall shape for the Northern hemisphere which the 6z has with its own 0z run, even at the outer stretches of medium range. If it's wrong on this (which is still likely at that range!) it's been very true to itself in terms of modelling.

    • Like 2
  2. 1 hour ago, Eagle Eye said:

    Polar Vortex is shrinking quickly on the forecasts and there's a large Baroclinic tilt especially the further up you go. Best indication I've seen of a potential split/major weakening yet but it's still just a forecast. The dynamical Tropopause linking up with the Strat Vortex appears to be ready for quite a large Wavebreaking event via Eddy's as mentioned in my post earlier but will it be enough for a major SSW? You really shouldn't ask me for that 😆. I'll try and learn a bit more about fluid dynamics over the next few days to see if I can get any closer to the answer. By then the GFS will have gone off the signal won't it 🤣.

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    Without wishing to pigeonhole your talents into purely the field of meteorology, if you do indeed wish in the future to pursue it as a career (and I think no-one here would have any doubts you've found a potential calling in it), I'll say this only because I haven't seen anyone else point it out yet (and it started bugging me solely because your posts are otherwise very high quality - keep them coming but keep on top of other subjects in class!)...

    An eddy (small 'e' works just fine, not like the name, referring to a vortex characteristic in a fluid), and eddies, (again small 'e').

    I say only because at some point in the future, you may wish to collate your postings as further evidence to submit to a university to which you may wish to apply. So, you really would want to use 'find and replace' to correct them.

    And about the models (and not in reply to Mr. Eagle Eye!)...

    I think we're going to see quite a few more days of disagreement in the 96-144 time period yet. Until perhaps another week or so has gone by. They're grappling with some pretty complex conundrums at the outer reaches of their ranges at the moment. Whether to form a Ural high / Aleutian low or not, how that then affects the stratosphere (i.e. severity, type and placement of the likely SSW), and then to extrapolate once again the knock-on effects from that in the troposphere, which in themselves, even with a QTR, are significantly further forward in time (min. 7-10 days beyond).

    In addition,  we have an atmosphere hopefully primed for a quick response to drivers (e.g. MJO) which could well bring about a pattern change to something more favourable (or not!).

    All in all, my thinking would be, it's still a little early to be hoping for the models to be settling down in these time frames. I mean, they're actually bl**dy good, but we do tend to keep demanding more from them and should keep in mind situations in which it's only natural output will be more chaotic.

    TL:DR... over-analysis between runs right now might be less productive than it is even normally! I think trends will be more useful, if they can be spotted.

    • Like 4
    • Thanks 2
  3. 3 hours ago, Mixer 85 said:

    Or to put it into a more useful, less alarming perspective, Greenland lost about 0.0058% of its total mass. At that rate it could disappear in just over 17,000years.

    I wouldn't trust that rate to stay the same... would you?

    Being on a bus right now with my phone, I'm consequently less able than usual to check on what's known about the historical rates over the last 100-or-so years. I'll bet others aren't hampered to the same degree, though, and could no doubt show an alarmingly growing trend in its rate of loss. Couple that with the reduced albedo due to the loss of sea ice across the entire Arctic area over roughly the same period, I think it's fair to say the balance of probability is pointing towards a less than rosy future in terms of sea levels.

    Not to mention, it really doesn't need to lose anything close to all of it to create a whole series of problems which are going to beset the grandchildren of our younger generation.

    As long as it's their problems and not ours, though, eh?

    • Like 2
  4. 4 hours ago, SqueakheartLW said:

    Maybe if the northwards trend of the azores high continues it'll end up so far north that it turns into a permanent northern blocking feature in the future.

    Me thinking a last straw attempt at getting northern blocking in the future and a faint hope that will bring cold in the future assuming there's any cold left to tap into that is.

    Maybe, but is it in fact trending N-wards or NE (seeming to find a more comfortable home over NW Europe)? The latter would not be in our favour...

  5. 1 hour ago, SLEETY said:

    does ukmo 168 every verify?????????

    Well, it must do, if ECM's 240 is being used to write off a whole ten days.

    Just to note though, I don't see anything particularly of a cold note in that period. However, that's because of the underlying drivers not being conducive, not so much the vagaries of the post-6-day det output.

    • Like 5
  6. 2 minutes ago, Lukesluckybunch said:

    ECM mean is terrible,nothing like the op.no sign of any heights building to northeast

    Which doesn't remove the op run from the range of possibilities, since it's run at a finer resolution and could be the very beginning of an indicator of a pattern change / new trend. If there are a range of clusters all pointing at different scenarios,  the mean is far less useful guidance. The building of heights NE is currently not yet a high probability outcome, taking purely the range of possibilities on offer. Its success will be highly dependent on how much the jet energy upstream ends up being routed further south, enabling the LP to establish centred around Italy. Need to keep HP out of W Europe, otherwise everything's riding over the top again.

    Better to check out the clusters (Catacol and Singularity often post them) and also check out what's going on upstream and with jet energy on the ensemble runs which either support the op or don't, to get an idea of how they are clustered and in which direction any mid-term trends (144 hrs+) may be moving.

    • Like 2
  7. On 25/12/2021 at 07:16, Weather-history said:

    Merry Christmas everyone and all the best to Michael Fish for the future

    To show just how good Michael Fish was as a BBC weather presenter, look at this short broadcast he had to put out on Christmas Eve 1999 and how much info he had to pack in, within 83 seconds. What a professional

     

    Indeed, not to mention the training and experience enabling the preparatory work behind each and every forecast, with consideration of level of technical detail, content and  tone, then the delivery itself with the various props available in the day. Michael Fish, a real British institution and what a well-earned retirement! Merry Christmas!

    • Like 3
  8. Just now, Nick B said:

    You'd be able to collate data on number of cold episodes. Our gut would tell us the expanded Hadley cell has been a strong factor. However, a 'failed initiation' from what point in time and from what kind of starting point? The various models are simply calculating from a starting point of right now and forecasting out to a future event which hasn't yet occurred, so what has initiated? Also, models have received numerous upgrades (usually but perhaps not always improvements) so we don't have a constant tool against which to measure the variance of outcomes over time. Could be problematic from that point of view.

     

  9. 2 hours ago, Kasim Awan said:

    Yes, but I would like to see more concrete research on the causal relationship between hadley cell expansion and uk winter synoptics such as the rate of failed initiation of cold with varying intensities of Hadley cell.

    You'd be able to collate data on number of cold episodes. Our gut would tell us the expanded Hadley cell has been a strong factor. However, a 'failed initiation' from what point in time and from what kind of starting point? The various models are simply calculating from a starting point of right now and forecasting out to a future event which hasn't yet occurred, so what has initiated? Also, models have received numerous upgrades (usually but perhaps not always improvements

    • Like 1
  10. 8 minutes ago, Kasim Awan said:

    If we can get some teamwork going between these 2 lows, disruption would easily lead to a frigid easterly by 250h (Xmas eve).

    gfs-0-234 (12).png

    Crucially, if it were to, we'd need it to continue to elongate and  deconstruct and not become a force for dragging warm uppers up into W. Europe from N. Africa. If that low is going to continue eastwards it needs to take a southerly trajectory to prop up the HP. However, it doesn't seem to have much of a jet to take it in any particular direction.

    • Like 1
  11. So, I have a question for the pro/semi-pros here. A week or two ago we were clearly in a pattern with seven waves in the northern hemisphere. The GFS looks to be moving that towards five (for what that's worth). Accuracy of any model's ability to handle this correctly aside, might we expect there to be more likelihood of brief interludes of (more) zonal weather during a transition of wave number such as that?

  12. 166bn tonnes. i.e. well over 2 million Queen Elizabeth aircraft carriers in mass. Or 500,000 Empire State Buildings. Or to compare it with a more relatively similar mass, it's about 1/6 of the weight of all man-made structures on the planet combined (about 1.1 trillion tonnes, which itself is now more than the weight of all the earth's biomass combined too). In one year.

  13. On 23/05/2018 at 21:39, JeffC said:

    Thanks...ever hopeful of seeing something of that ilk in my lifetime...if I recall correctly Mr St Helens famous eruption in 1980 did have some impact..(?)

    Pinatubo's in 1991 was assessed to have brought down global temperatures by 0.5 Deg C from 1991 to 1993 or so.  That was a VEI 6 and about 10 times the size of Mt. St. Helens in terms of ejecta, ejecting its ash up to 34km (21 miles) high at its peak, well into the stratosphere. Pretty substantial. Would be nice if nature could display without threatening peoples' lives, homes, livelihoods and also local ecosystems, however, events of this magnitude are always going to leave casualties. Impressive but sadly catastrophic too.

  14. 1 hour ago, JeffC said:

    Maybe too early to tell, but is there any scope for the Kilauea eruption to affect short-medium term weather locally and /or globally? 

    Very unlikely. This would need to be VEI 6 (+) and ejecting the plume well into the stratosphere. Kilauea is not likely to meet those criteria.

    • Thanks 1
  15. No point in moaning about the weather - it's not going to change it.  The only thing which can be improved is how you view it.  Almost all weathers to extremes can cause harm in some way - heat, cold, not enough sunlight, too much rain, not enough rain, ice, deep impenetrable snow, hard frost, wind etc. etc. Luckily, for our part of the world, few of them last for any really appreciable length of time (up until now in this historical era).  Some of them could even be mitigated to some extent if there was a reasonable functioning system of governance in place (fairer system of fuel payments, long term water use planning etc.).

  16. As a layperson, I'd say those are both possibilities to some extent, in that several recorded SSW have occurred, however no two are that much alike.  So, yes, perhaps a difficulty for those who have to write the programming for the models is how much emphasis to give the myriad of factors when there is limited data from previous events upon which to base those emphases.

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