Titlebook: Atmospheric Computations to Assess Acidification in Europe; Summary and Conclusi Joseph Alcamo,Jerzy Bartnicki Book 1989 Kluwer Academic Pu

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CERE

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HAWK

978-94-010-6904-5Kluwer Academic Publishers 1989

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Timed und stochastische Petri-Netze,e FAST method requires frequency distribution of model parameters as input data and provides the following results: (i) mean value of the model output, (ii) variance of the model output which characterizes the parameter uncertainty of the model, and (iii) partial variances of the model output which

周興旺

https://doi.org/10.1007/978-3-642-83801-9 of ‘coarse’ boundary values (provided by a coarse-grid model) in the fine-grid model is discussed theoretically and demonstrated by test calculations. It turns out that one should always prefer applying coarse information about external (with respect to the fine-grid model) sources to ignoring them

sorbitol

https://doi.org/10.1007/978-3-642-83801-9t runs on a personal computer (RCDM) using an extended period of wind and precipitation data. The variability in historical temperature and precipitation data has been analyzed to assess the representativeness of the limited meteorological period used in the EMEP model (1978–1982). A match-up betwee

排出

Funktionale Grammatik und Sprachbeschreibunger the same period. The basis for classifying different types of atmospheric circulation or large-scale weather paterns [commonly known as Grosswettertypes (GWT-s) or Grosswetterlagen (GWL-n)] is the identification of the position of centers of cyclones, ridges and troughs. The linear regression bet