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Philip T. Bergmaier and Bart Geerts

about the fall speed estimates and their uncertainties are discussed in appendix A . Fig . 1. (a) WRF Model domains, and (b) regional map of Lake Ontario showing relevant locations and geographic features discussed throughout the text. b. Dual-Doppler synthesis Radial velocity measurements from the two downward-pointing WCR beams were used to retrieve the 2D wind field in the vertical plane below the UWKA via an airborne dual-Doppler (DD) synthesis technique described by Leon et al. (2006) and

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Scott M. Steiger, Tyler Kranz, and Theodore W. Letcher

, J. , N. Pineda , T. Rigo , and M. Aran , 2013 : Remote sensing analysis of a Mediterranean thundersnow and low-altitude heavy snowfall event . Atmos. Res. , 123 , 305 – 322 , https://doi.org/10.1016/j.atmosres.2012.06.021 . 10.1016/j.atmosres.2012.06.021 Cummins , K. L. , and M. J. Murphy , 2009 : An overview of lightning locating systems: History, techniques, and data uses, with an in-depth look at the U.S. NLDN . IEEE Trans. Electromagn. Compat. , 51 , 499 – 518

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