On the eastern side of the aforementioned blocking anticyclone a parade of troughs that had crested this anticyclone dropped south-southeastward toward a persistent trough that was situated across eastern Iran, Afghanistan, Pakistan, and the Tibetan Plateau. A persistent quasi-stationary 700-hPa cutoff cyclone associated with this trough was located on the border of Pakistan and India. This cutoff cyclone facilitated the northeastward transport of very moist air (precipitable water values > 60 mm and integrated water vapor transport values > 1000 kg/m/s) across the Arabian Sea toward western India and from there northwestward toward Pakistan. Preliminary evidence suggests that the aforementioned moist southwesterly flow across the Arabian Sea was enhanced by a merger with a westward-directed equatorial flow of very moist air from the tropical western Pacific Ocean. Preliminary evidence also suggests that the extraordinary heavy rains that fell across Pakistan were associated more with duration than with rainfall intensity, given the large-scale “flow constipation” that persisted from eastern Europe to western Asia during much of August 2022. The key player in the aforementioned “flow constipation” process was an unusually persistent, high-amplitude, quasi-stationary ridge centered over eastern Europe and western Russia.
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