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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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#1
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I could be completely wrong but I don't see how you can take a mean of
different evolutions. For example, in the GFS 850 hPa ensembles for Feb 28th there are 4 members around +3C and six around 5-10C giving a mean about -4C. Isn't this a bit like saying the mean of a warm sunny day and a cold snowy day is an average cloudy day. Surely one type of synoptic evolution will prevail and it is the mean within that particular evolution which is likely to provide the best outcome. So that would mean February 28th is likely to have max temperatures of around, say, 4 deg C or 10 deg C depending on the resulting evolution. Not the mean of 7C. Please correct me if this is not basically correct. Dave |
#2
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![]() "Dave.C" wrote in message k... I could be completely wrong but I don't see how you can take a mean of different evolutions. Although this page deals with EC output, the basic principle is the same .... http://www.ecmwf.int/products/foreca...mble_mean.html It is acknowledged that you shouldn't just look at the mean of the ensemble; in the EC output, with many more members, then sophisticated analysis of the 'clustering' is performed, and it is these rather than the crude mean solution that is used to assess the likelihood of future developments. I use the mean on the GFS output simply as a 'eyeball guiding' line (to judge how the outcomes are clustering about it) rather than trying to use it to explicitly work out the future state of the atmosphere. It's not a 'fallacy', just another tool. Martin. -- FAQ & Glossary for uk.sci.weather at:- http://homepage.ntlworld.com/booty.weather/uswfaqfr.htm and http://booty.org.uk/booty.weather/metindex.htm |
#3
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In article ,
Dave.C writes: I could be completely wrong but I don't see how you can take a mean of different evolutions. For example, in the GFS 850 hPa ensembles for Feb 28th there are 4 members around +3C and six around 5-10C giving a mean about -4C. Isn't this a bit like saying the mean of a warm sunny day and a cold snowy day is an average cloudy day. Surely one type of synoptic evolution will prevail and it is the mean within that particular evolution which is likely to provide the best outcome. So that would mean February 28th is likely to have max temperatures of around, say, 4 deg C or 10 deg C depending on the resulting evolution. Not the mean of 7C. Please correct me if this is not basically correct. I think you are right, but I suppose a simple mean has the advantage of simplicity. Most of the time, the ensemble members will probably be spread fairly uniformly about the mean, with the bi-modal situation that you've identified being the exception rather than the rule. In any case, so long as you aren't only provided with the mean, with the individual members being hidden, then I don't see that there's a problem, Another point is that I believe that the "operational run" is calculated on a finer grid than the other members, so arguably should be given more weight when calculating the mean. -- John Hall "Honest criticism is hard to take, particularly from a relative, a friend, an acquaintance, or a stranger." Franklin P Jones |
#4
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![]() Another point is that I believe that the "operational run" is calculated on a finer grid than the other members, so arguably should be given more weight when calculating the mean. I don't suppose you know if it is, do you John? Thanks, Dave |
#5
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In article ,
Dave.C writes: Another point is that I believe that the "operational run" is calculated on a finer grid than the other members, so arguably should be given more weight when calculating the mean. I don't suppose you know if it is, do you John? Given more weight? I don't think so, but that's only based on eyeballing the ensemble graphs. -- John Hall "Honest criticism is hard to take, particularly from a relative, a friend, an acquaintance, or a stranger." Franklin P Jones |
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