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Adam C. Varble, Stephen W. Nesbitt, Paola Salio, Joseph C. Hardin, Nitin Bharadwaj, Paloma Borque, Paul J. DeMott, Zhe Feng, Thomas C. J. Hill, James N. Marquis, Alyssa Matthews, Fan Mei, Rusen Öktem, Vagner Castro, Lexie Goldberger, Alexis Hunzinger, Kevin R. Barry, Sonia M. Kreidenweis, Greg M. McFarquhar, Lynn A. McMurdie, Mikhail Pekour, Heath Powers, David M. Romps, Celeste Saulo, Beat Schmid, Jason M. Tomlinson, Susan C. van den Heever, Alla Zelenyuk, Zhixiao Zhang, and Edward J. Zipser

-level flow often switched to southeasterly, commonly behind MCSs or cold fronts, where stable, moist, and relatively low CCN concentrations supported warm rain formation or drizzling fog. Above this stable layer, northerly flow commonly continued to advect in warm, moist air, sometimes for a day or more, feeding elevated deep convection decoupled from the surface. Fig . 6. Low-level (a) zonal wind (positive toward the east), (b) meridional wind (positive toward the north; color fill) with microwave

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