The Interaction between Very Deep Convection and Biomass Burning Plumes during DC3 and the Impact on the UTLS Region over The North Atlantic
Heidi Huntrieser1, Michael Lichtenstern1, Monika Scheibe1, Heinfried Aufmhoff1, Hans Schlager2, Katharina Heimerl1, Tomas Pucik1, Andreas Minikin1, Bernadett Weinzierl3, Daniel Fütterer1, Ilana B Pollack4, Jeff Peischl5, Thomas B Ryerson6, Shawn Bryan Honomichl7, Johnathan W Hair8, Carolyn F Butler8, Michael J Schwartz9, Bernhard Rappenglück10, Luis Ackermann10, Kenneth E Pickering11, Kristin Cummings12, Michael I Biggerstaff13, Daniel Betten13 and Mary C Barth14, (1)German Aerospace Center (DLR), Institute of Atmospheric Physics, Oberpfaffenhofen, Germany, (2)German Aerospace Center (DLR), Oberpfaffenhofen, Germany, (3)University of Vienna, Vienna, Austria, (4)Colorado State University, Department of Atmospheric Science and Department of Chemistry, Fort Collins, CO, United States, (5)Cooperative Institute for Research in Environmental Sciences, Boulder, United States, (6)NOAA ESRL Chemical Sciences Division, Tropospheric Chemistry Program, Boulder, CO, United States, (7)National Center for Atmospheric Research, Boulder, CO, United States, (8)NASA Langley Research Center, Hampton, VA, United States, (9)NASA Jet Propulsion Laboratory, Pasadena, CA, United States, (10)University of Houston, Department of Earth & Atmospheric Sciences, Houston, TX, United States, (11)NASA Goddard Space Flight Center, Greenbelt, MD, United States, (12)University of Maryland College Park, College Park, MD, United States, (13)University of Oklahoma Norman Campus, Norman, OK, United States, (14)National Center for Atmospheric Research, Boulder, United States
