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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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#11
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John Dann wrote:
On Fri, 25 Sep 2009 08:47:53 +0100, "Will Hand" wrote: Put simply - chaos in action! If I might be permitted a small hobby-horse aside here, I do wish this word chaos had never become associated with atmospheric modelling. To my way of thinking, this behaviour is not chaotic at all, it's sensitive, or super/hyper-sensitive if you will (to the starting conditions). Chaotic - to me - implies irrational or unknowable, which is not what's happening here. Once you can define the starting conditions with sufficient accuracy then the models can indeed run with a rational outcome and so aren't chaotic. JGD I think the word chaos is used because so many of the important processes taking place in the atmosphere are at scales that are orders of magnitude smaller than can be resolved by the numerical models, at least the global and regional models. If it can't be adequately modelled then it does appear chaotic Norman |
#12
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![]() "Norman" wrote in message ... John Dann wrote: On Fri, 25 Sep 2009 08:47:53 +0100, "Will Hand" wrote: Put simply - chaos in action! If I might be permitted a small hobby-horse aside here, I do wish this word chaos had never become associated with atmospheric modelling. To my way of thinking, this behaviour is not chaotic at all, it's sensitive, or super/hyper-sensitive if you will (to the starting conditions). Chaotic - to me - implies irrational or unknowable, which is not what's happening here. Once you can define the starting conditions with sufficient accuracy then the models can indeed run with a rational outcome and so aren't chaotic. JGD I think the word chaos is used because so many of the important processes taking place in the atmosphere are at scales that are orders of magnitude smaller than can be resolved by the numerical models, at least the global and regional models. If it can't be adequately modelled then it does appear chaotic Norman Chaos is a mathematical theory. Very simple looking equations can be chaotic, i.e. miniscule changes in starting numbers can produce vast differences very quickly. The Navier Stokes equations used to model the atmosphere, I don't think are themselves chaotic, but they have no precise analytical solution and so approximations have to be made using grids of data. This introduces chaotic behaviour. Finer grids are not the ultimate answer as errors can amplify more quickly then. There is a limit to deterministic predictability with NWP, there will also be a limit to statistical (ensemble) prediction as well, nobody is sure where those limits are but they are there just the same. Some say 10 days, some say further ahead before you get into climatology and dominant signals forced by physics. HTH. Will -- |
#13
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On Sep 25, 8:47*am, "Will Hand" wrote:
"Dawlish" wrote in message ... On Sep 24, 1:46 pm, Dawlish wrote: On Sep 23, 7:20 pm, "Keith(Southend)" wrote: Seems to be consistency in all the models for a northerly plunge next week as we enter the month of October. September is turning out another very dry month here in Southend-on-Sea, with currently only 8.0mm of rain (17% average), as it stands it will be second driest after 1997 (7.6mm), 1985 (9.7mm, 3rd driest) temperatures are also standing at 1.0°C above average. -- Keith (Southend)http://www.southendweather.net e-mail: kreh at southendweather dot net There certainly *was* Keith! I find the turn of events over this last week really interesting. 6 days ago, the models picked up the re-establishment of the high pressure. The consistency and agreement was enough for me to forecast at 10 days and barring something very strange, that forecast looks as if it will be good. However, a short time after my forecast for the 29th, the ECM massively, then, to a lesser extent, the gfs showed a northerly, which is likely not to occur. This "faux-northerly" stayed on the charts for a couple of days and then over the last 36 hours has been erased. ===================== Paul, thank goodness it is not February, else you would see toys and tipped over prams everywhere by now! For me, substitute February for December and/or January. Bright and mild weather in Feb is not at all unpleasant, it makes it seem like spring has arrived (which, if one uses the criterion of winter being the darkest three months, it has). On the other hand in Dec and Jan, the cold and the snow are much more essential for aesthetic appeal, there's little worse than endless dark, damp, drizzly days.... Nick |
#14
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On Sep 25, 9:36*am, John Dann wrote:
On Fri, 25 Sep 2009 08:47:53 +0100, "Will Hand" wrote: Put simply - chaos in action! If I might be permitted a small hobby-horse aside here, I do wish this word chaos had never become associated with atmospheric modelling. To my way of thinking, this behaviour is not chaotic at all, it's sensitive, or super/hyper-sensitive if you will (to the starting conditions). Chaotic - to me - implies irrational or unknowable, which is not what's happening here. Once you can define the starting conditions with sufficient accuracy then the models can indeed run with a rational outcome and so aren't chaotic. JGD The term Chaos is quite appropriate to atmospheric modelling because no matter how accurately the starting conditions are defined (even down to the molecular level) the detailed state of the system after a certain length of time is literally unknowable. That length of time is less than a month, as far as I know. This behaviour is called deterministic chaos because each successive condition depends on the previous one but no-one can say which path the system will evolve along. The individual infinitesimal steps in the process are rational but the final outcome is not. Tudor Hughes, Warlingham, Surrey. |
#15
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On Fri, 25 Sep 2009 11:38:53 +0100, "Will Hand"
wrote: "Norman" wrote in message ... John Dann wrote: On Fri, 25 Sep 2009 08:47:53 +0100, "Will Hand" wrote: Put simply - chaos in action! If I might be permitted a small hobby-horse aside here, I do wish this word chaos had never become associated with atmospheric modelling. To my way of thinking, this behaviour is not chaotic at all, it's sensitive, or super/hyper-sensitive if you will (to the starting conditions). Chaotic - to me - implies irrational or unknowable, which is not what's happening here. Once you can define the starting conditions with sufficient accuracy then the models can indeed run with a rational outcome and so aren't chaotic. JGD I think the word chaos is used because so many of the important processes taking place in the atmosphere are at scales that are orders of magnitude smaller than can be resolved by the numerical models, at least the global and regional models. If it can't be adequately modelled then it does appear chaotic Norman Chaos is a mathematical theory. Very simple looking equations can be chaotic, i.e. miniscule changes in starting numbers can produce vast differences very quickly. The Navier Stokes equations used to model the atmosphere, I don't think are themselves chaotic, but they have no precise analytical solution and so approximations have to be made using grids of data. This introduces chaotic behaviour. Finer grids are not the ultimate answer as errors can amplify more quickly then. There is a limit to deterministic predictability with NWP, there will also be a limit to statistical (ensemble) prediction as well, nobody is sure where those limits are but they are there just the same. Some say 10 days, some say further ahead before you get into climatology and dominant signals forced by physics. HTH. Will Hi Will, I am not sure why you used the term statistical and ensemble together here as ensembles of dynamic models are used in a probabilistic framework. Is this what you were calling statistical models as it is a term that is more often associated with empirical models e.g. those that directly correlate rainfall over a region with SSTs etc. Andy |
#16
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![]() "Andy" wrote in message ... On Fri, 25 Sep 2009 11:38:53 +0100, "Will Hand" wrote: "Norman" wrote in message ... John Dann wrote: On Fri, 25 Sep 2009 08:47:53 +0100, "Will Hand" wrote: Put simply - chaos in action! If I might be permitted a small hobby-horse aside here, I do wish this word chaos had never become associated with atmospheric modelling. To my way of thinking, this behaviour is not chaotic at all, it's sensitive, or super/hyper-sensitive if you will (to the starting conditions). Chaotic - to me - implies irrational or unknowable, which is not what's happening here. Once you can define the starting conditions with sufficient accuracy then the models can indeed run with a rational outcome and so aren't chaotic. JGD I think the word chaos is used because so many of the important processes taking place in the atmosphere are at scales that are orders of magnitude smaller than can be resolved by the numerical models, at least the global and regional models. If it can't be adequately modelled then it does appear chaotic Norman Chaos is a mathematical theory. Very simple looking equations can be chaotic, i.e. miniscule changes in starting numbers can produce vast differences very quickly. The Navier Stokes equations used to model the atmosphere, I don't think are themselves chaotic, but they have no precise analytical solution and so approximations have to be made using grids of data. This introduces chaotic behaviour. Finer grids are not the ultimate answer as errors can amplify more quickly then. There is a limit to deterministic predictability with NWP, there will also be a limit to statistical (ensemble) prediction as well, nobody is sure where those limits are but they are there just the same. Some say 10 days, some say further ahead before you get into climatology and dominant signals forced by physics. HTH. Will Hi Will, I am not sure why you used the term statistical and ensemble together here as ensembles of dynamic models are used in a probabilistic framework. Is this what you were calling statistical models as it is a term that is more often associated with empirical models e.g. those that directly correlate rainfall over a region with SSTs etc. To me ensemble prediction is a form of statistical prediction as one uses the ensemble mean and the members to determine the probability of an event occuring. Of course correlation techniques are also statistical as you say. Cheers, Will -- |
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