• dynamic meteorology;
  • communication;
  • general circulation;
  • the Coriolis Effect;
  • education;
  • rotation;
  • common sense.


The problems of communicating essential processes in dynamic meteorology are discussed, with examples. It is argued that the difficulty in conveying the concepts is not a result of the non-linearity of atmospheric and ocean motions, but their counter-intuitive nature. Although this might motivate the highly mathematical way dynamic meteorology is communicated, issues arise when the mathematics is poorly or wrongly interpreted. It is suggested that communication would be improved by laboratory experiments and observational evidence, while an historical background could help explain why a particular phenomenon is important. © Crown Copyright 2010. Reproduced with the permission of the Controller of HMSO. Published by John Wiley & Sons, Ltd