Katabatically Driven Downslope Windstorm-Type Flows on the Inner Sidewall of Arizona's Barringer Meteorite Crater
Charles D Whiteman1, Manuela Lehner2, Sebastian W Hoch1, Matthew Hills1, Thomas Haiden3, Iris Feigenwinter4, Martina Grudzielanek5, Mateja Maric6, Norbert Kalthoff7, Roland Vogt4, Jan Cermak5, Richard Rotunno8, Ronald Calhoun9, Nihanth Wagmi Cherukuru10 and Bianca Adler11, (1)University of Utah, Atmospheric Sciences, Salt Lake City, UT, United States, (2)University of Innsbruck, Innsbruck, Austria, (3)European Center for Medium Range Weather Forecasting, Reading, United Kingdom, (4)University of Basel, Basel, Switzerland, (5)Ruhr University Bochum, Bochum, Germany, (6)Ruhr Universität Bochum, Bochum, Germany, (7)Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research - Troposphere Research(IMK-TRO), Karlsruhe, Germany, (8)National Center for Atmospheric Research, Mesoscale & Microscale Meteorology Division, Boulder, CO, United States, (9)Arizona State University, Tempe, AZ, United States, (10)National Center for Atmospheric Research, Boulder, United States, (11)Karlsruhe Institute of Technology (KIT), Institute of Meteorology and Climate Research (IMK-TRO), Eggenstein-Leopoldshafen, Germany
