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Original Articles

On the contrasting influence of organized moist convection and surface heat flux on a barotropic vortex

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Pages 385-389 | Received 23 Jun 1986, Accepted 27 Nov 1986, Published online: 15 Dec 2016

References

  • Aakjær, P. and Rasmussen, E. 1985. Modelling of polar lows in a barotropic environment using the Danish operational limited area model. Report No. 6, Weather Service, Danish Meteorological Institute, Copenhagen, SO p.
  • Bratseth, A. M. 1985. A note on CISK in polar air masses. Tellus37A, 403–406.
  • Lorenz, E. N. 1960. Energy and numerical weather prediction. Tellus12, 364–373.
  • Økland, H. 1987. Heating by organized convection as a Tellus 39A (1987), 4 source of polar low intensification. Tellus 39A, 398–408.
  • Rasmussen, E. 1979. The polar low as an extratropical CISK-disturbance. Q. J. R. Meteorol. Soc. 105, 531–549.
  • Schubert, W. H., Wakefield, J. S., Steiner, E. J. and Cox, S. K. 1979. Marine stratocumulus convection. Part II: Horizontally inhomogeneous solutions. J. Atmos. Sci. 36, 1308–1324.