By Wiesner, Clarence Jack
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Additional resources for Hydrometeorology
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The variability in predictability of deep convection has been studied by Done et al. (2012). Indeed, convection is not necessarily a vertical process. 2. The potential energy (energy arising from moving a parcel to a greater height against gravity) of the system does not change, and movement from B to C requires energy to raise the centre of gravity of the parcel upwards, as in the movement of the parcel of air discussed so far. However, movement from A to D could cause the centre of gravity of the parcel to be lowered, causing energy to be released.
21, 455–465. J. L. (2012) Under what conditions does embedded convection enhance orographic precipitation? Q. J. R. Meteorol. , 138, 391–406. N. (1980) Airflow through mid‐latitude cyclones and the comma cloud pattern. Mon. , 108, 1498–1509. Caylor, I. and Illingworth, A. (1987) Radar observations and modelling of warm rain initiation. Q. J. R. Meteorol.