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An extended version of the Q-vector form for the ω-equation that includes diabatic (in particular latent) heating in the Q-vector itself is derived and tested for use in analyzing the life-cycle of a midlatitude cyclone that developed over the central United States during 24–26 December 2009.  While the inclusion of diabatic heating in the Q-vector ω-equation is not unique to this work, the inclusion of diabatic heating in the Q-vector itself is a unique formulation.  Here it is shown that the diabatic Q-vector gives a better representation of the forcing contributing to the life-cycle of the Christmas Storm of 2009 using analyses derived from the 80-km NAM

advances in meteorology

The Application of Diabatic Heating in<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" id="M1"><mml:mrow><mml:mi>Q</mml:mi></mml:mrow></mml:math>-Vectors for the Study of a North American Cyclone Event

The Application of Diabatic Heating inQ-Vectors for the Study of a North American Cyclone Event