Lifecycle‐Type Matters for Extratropical Cyclone Precipitation Production

In the midlatitudes, extratropical cyclones produce the majority of winter precipitation. Precipitation rates and accumulation depend strongly on both the cyclone intensity and the environmental moisture amount. Using 5 years of the Integrated Multi‐satellitE Retrievals for Global Precipitation Measurement (IMERG) product, cyclone‐centered composites of surface precipitation rates are compared between cyclones that occlude and those that do not. Occluding cyclones produce greater surface precipitation because they tend to be more intense. When the non‐occluding cyclones are selected such that they collectively have similar intensity and moisture amount distributions as the occluding cyclones, precipitation rates at peak intensity are still larger for occluding cyclones. This is because a particular type of forced, frontal‐scale, ascent in the occluded thermal ridge, unique to occluded cyclones by virtue of their thermal structure, favors more precipitation. The results demonstrate that life‐cycle type (i.e., achieving occlusion vs. not) matters for precipitation production in extratropical cyclones. Plain Language Summary The weather in the midlatitudes is driven by extratropical cyclones and these storms produce most of the winter precipitation in the northern hemisphere. Both the intensity of the cyclones and the amount of moisture available to them determine how much precipitation they will produce. However, using satellite observations of precipitation averaged in cyclones, it is discovered that the lifecycle‐ type and associated structural evolution of the cyclones also impacts the precipitation production. Cyclones that undergo occlusion are found to be associated with greater precipitation production than cyclones that do not occlude when the comparison is controlled for similar cyclone intensity and moisture amount. This is because the occluded cyclones are characterized by additional forcing for ascent that boosts precipitation production at the frontal scale. Therefore lifecycle type matters for the amount of precipitation cyclones produce.