core.ac.uk · the fgge 111b grid point data of 12 gmt 7 july 1979 were used as input to the model...

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Page 1: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 2: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 3: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 4: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 5: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 6: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 7: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 8: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 9: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 10: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 11: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 12: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 13: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 14: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 15: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 16: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense
Page 17: core.ac.uk · The FGGE 111b grid point data of 12 GMT 7 July 1979 were used as input to the model for all numerical experimentations. The dominant synoptic feature was an intense