Editing 1885: Ensemble Model

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The first three outcomes are real while the others are less serious. They are explained below:
 
The first three outcomes are real while the others are less serious. They are explained below:
;…rain is 0.5% more likely in some areas …wind speeds are slightly lower …pressure levels are randomly tweaked
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;…rain is 0.5% more likely in some areas
These realistic outcomes are only possible under calm weather conditions. Predicting these values with an accuracy better than 1% indicates that the model is stable even when the ''initial conditions'' are slightly changed. Modern weather forecasts at normal circumstances are often not good as this and for a hurricane or tornado the variances are much higher.
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Historical rain data are used to estimate the probability of rainstorms of a certain size and duration occurring, e.g. the {{w|Flood Studies Report|Flood Studies Report}} in the UK. Randall here is suggesting that an alternate universe exists where these estimates are higher (and presumably lower) in some areas, and that the estimates of rainfall in this alternate universe is accounted for within ensemble modelling in our own universe. This sort of change in prediction is frequently used when accounting for 'worst case scenarios' in the design processes of structures such as dams. However, the figures to the left appear to indicate time-dependent models, which are typically physics based, e.g. {{w|Large eddy simulation|Large Eddy Simulation}} models or other atmospheric process based models. In those sorts of models, likelihood of rain is usually a prediction rather than a parameter, but might be used as a parameter in a second iteration.
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;…wind speeds are slightly lower
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A usual parameter.
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;…pressure levels are randomly tweaked
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A very vague but otherwise understandable parameter.
  
 
;…dogs run slightly faster
 
;…dogs run slightly faster

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