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Julia H. Keller, Christian M. Grams, Michael Riemer, Heather M. Archambault, Lance Bosart, James D. Doyle, Jenni L. Evans, Thomas J. Galarneau Jr., Kyle Griffin, Patrick A. Harr, Naoko Kitabatake, Ron McTaggart-Cowan, Florian Pantillon, Julian F. Quinting, Carolyn A. Reynolds, Elizabeth A. Ritchie, Ryan D. Torn, and Fuqing Zhang

, S. , D. M. Schultz , and G. Vaughan , 2017a : Early evolution of the 23–26 September 2012 U.K. Floods: Tropical Storm Nadine and diabatic heating due to cloud microphysics . Mon. Wea. Rev. , 145 , 543 – 563 , https://doi.org/10.1175/MWR-D-16-0200.1 . 10.1175/MWR-D-16-0200.1 Hardy , S. , D. M. Schultz , and G. Vaughan , 2017b : The 23–26 September 2012 U.K. Floods: Using PV surgery to quantify sensitivity to upper-level forcing . Mon. Wea. Rev. , 145 , 4055 – 4079 , https

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Volkmar Wirth, Michael Riemer, Edmund K. M. Chang, and Olivia Martius

and E have been created during that time. c. Different types of RWPs and their propagation There are different types of RWPs associated with different temporal and spatial scales, different types of forcing, and specific properties of the background flow. Sometimes an RWP is little more than an individual trough or ridge ( Sanders 1988 ); sometimes an RWP may span a substantial part of the globe ( Branstator 2002 ). Some RWPs propagate along great circles, while others are ducted in the zonal

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