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Short Contribution

On the determination of the predictability of a four-level geostrophic model using the effects of grid point numerical errors

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Pages 588-592 | Received 20 Apr 1976, Accepted 22 Apr 1977, Published online: 15 Dec 2016

References

  • Charney, J. G. 1965. A global experiment. Dynamics of large scale processes. Proceedings of the International Symposium in Moscow, June 23-30, 1%5 (edited by A. S. Monin), pp. 21-35.
  • Everson, P. J. and Davies, D. R. 1971. A note on the dependence of atmospheric predictability on baro-clinic development. Q. J. Roy. Met. Soc. 97, No. 412, 238–241.
  • Phillips, N. A. 1956. The general circulation of the atmosphere: A numerical experiment. Q. J. Roy. Met. Soc. 82, No. 352,123-164.
  • Searle, J. W. and Davies, D. R. 1975a. The sensitivity of dependence of large scale flow characteristics in a four-level model atmosphere on a simulated planetary boundary layer. Tellus 27, 145–154.
  • Searle, J. W. and Davies, D. R. 1975b. A note on the effect of grid point numerical errors on the large scale flow characteristics of a four-level model of the atmos-phere. Tellus 27,155-156.
  • Smagorinsky, J., Miyakoda, K. and Strickler, R. F. 1970. The relative importance of variables in initial con-ditions for dynamic weather prediction. Tellus 22, 141–157.
  • Williamson, D. L. and Washington, W. M. 1973. On the importance of precision for short range forecasting and climate simulation. J. Appl. Meteorol. 12, No. 8, 1254–1258.