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H. F. Dacre, P. A. Clark, O. Martinez-Alvarado, M. A. Stringer, and D. A. Lavers

formation of high TCWV bands in the atmosphere. This is achieved by calculating the water vapor budget for each cyclone in a frame of reference that moves with the cyclone. This allows us to determine how processes leading to the formation of atmospheric rivers evolve as the cyclone develops. Furthermore, tracking the cyclones relative to their time of maximum intensity allows us to composite the water vapor budget for a whole climatology of cyclones and thus generalize our results beyond individual

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