SUMMARYA method suggested earlier by the author to determine turbulent fluxes of heat and momentum from a measured wind profile is tested by using Swinbank's observational data.
Is atmospheric dispersion forecasting an important asset of the early-phase nuclear emergency response management? Is there a 'perfect atmospheric dispersion model'? Is there a way to make the results of dispersion models more reliable and trustworthy? While seeking to answer these questions the multi-model ensemble dispersion forecast system ENSEMBLE will be presented.
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