C21D:
Dust, Black Carbon, and Other Aerosols in the Cryosphere II
Session ID#: 10893
Session Description:
Recent observation and modeling efforts have established the powerful region impacts on snow and ice cover from the deposition of light absorbing impurities such as mineral dust and carbonaceous particles. The subsequent darkening of the snow surface and initiation of snow albedo feedbacks has implications for the global climate and water cycle. This session will focus on observations and modeling of the past, present, and future impacts of dust, carbonaceous particles, and other aerosols on snow and ice cover including transport and deposition processes, snowmelt, glacier/ice sheet mass balance, and atmospheric heating.
Primary Convener: McKenzie Skiles, NASA Jet Propulsion Laboratory, Pasadena, CA, United States
Conveners: Thomas H Painter, NASA Jet Propulsion Laboratory, Pasadena, CA, United States, Mark Flanner, University of Michigan Ann Arbor, Climate and Space Sciences and Engineering, Ann Arbor, MI, United States and John Faulkner Burkhart, University of Oslo, Geosciences, Oslo, Norway; University of California, Merced, Sierra Nevada Research Institute, Merced, CA, United States
Chairs: McKenzie Skiles, NASA Jet Propulsion Laboratory, Pasadena, CA, United States and Thomas H Painter, NASA Jet Propulsion Laboratory, Pasadena, CA, United States
OSPA Liaison: McKenzie Skiles, NASA Jet Propulsion Laboratory, Pasadena, CA, United States
Cross-Listed:
Abstracts Submitted to this Session:
Penny M Rowe1, Raul Cordero1, Stephen G Warren2, Alec Pankow3, José Jorquera1, Michael Schrempf4, Sarah J Doherty5, Marta Cabellero1, Jorge F Carrasco6 and Steven Neshyba7, (1)Universidad de Santiago de Chile, Santiago, Chile, (2)Univ Washington, Seattle, WA, United States, (3)University of Puget Sound, Tacoma, WA, United States, (4)Institut für Meteorologie und Klimatologie, Hannover, Germany, (5)University of Washington, Department of Atmospheric and Climate Science, Seattle, United States, (6)Organization Not Listed, Washington, DC, United States, (7)University Puget Sound, Tacoma, WA, United States
Julia Schmale1,2, Mark Flanner3, Shichang Kang4, Michael Sprenger5, Qianggong Zhang6,7, Yang Li6,7, J. Guo6,7 and Margit Schwikowski8, (1)Paul Scherrer Institute, Villingen, Switzerland, (2)Institute for Advanced Sustainability Studies, Potsdam, Germany, (3)University of Michigan Ann Arbor, Climate and Space Sciences and Engineering, Ann Arbor, MI, United States, (4)ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China, (5)ETH Zurich, Institute for Atmospheric and Climate Science, Zurich, Switzerland, (6)State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute (CAREERI), Chinese Academy of Sciences (CAS), Lanzhou, China, (7)Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Lanzhou, China, (8)Paul Scherrer Institute, Center for Energy and Environmental Sciences, Villingen, Switzerland
Ling Qi, Univ of California Los Angeles, Los Angeles, CA, United States, Qinbin Li, UCLA, Los Angeles, CA, United States, Dr. Cenlin He, NSF National Center for Atmospheric Research (NCAR), Research Applications Laboratory, Boulder, United States and Yinrui Li, Peking University, School of Physics, Beijing, China
Felix Matt1, John Faulkner Burkhart1,2 and Joni-Pekka Pietikäinen3, (1)University of Oslo, Geosciences, Oslo, Norway, (2)University of California, Merced, Sierra Nevada Research Institute, Merced, CA, United States, (3)Finnish Meteorological Institute, Helsinki, Finland
Ben Livneh, University of Colorado at Boulder, Department of Civil, Environmental, and Architectural Engineering, Boulder, United States, Jeffrey S Deems, National Snow and Ice Data Center, Boulder, CO, United States, Brian Buma, University of Alaska Southeast, Forest Ecosystem Ecology, Juneau, AK, United States, Joseph J Barsugli, CIRES, Boulder, CO, United States, Dominik Schneider, University of Colorado at Boulder, Geography / INSTAAR, Boulder, CO, United States, Noah P Molotch, University of Colorado at Boulder, Geography / INSTAAR, Boulder, United States, Carol Adele Wessman, University of Colorado at Boulder, EBIO, Boulder, CO, United States and Klaus Wolter, University of Colorado at Boulder, CIRES, Boulder, CO, United States
Yun Qian1, Sarah J Doherty2, William K-M Lau3, Jing Ming4, Hailong Wang1, Stephen G Warren5, Dr. Teppei J Yasunari, PhD6, Rudong Zhang7 and Mark Flanner8, (1)Pacific Northwest National Laboratory, Richland, WA, United States, (2)University of Washington, Department of Atmospheric and Climate Science, Seattle, United States, (3)Earth System Science Interdisciplinary Center, College PARK, United States, (4)National Climate Center, Chinese Meteorological Administration, Beijing, China, (5)Univ Washington, Seattle, WA, United States, (6)Hokkaido University, Arctic Research Center, Sapporo, Japan, (7)Nanjing University, School of Atmospheric Sciences, Nanjing, China, (8)University of Michigan Ann Arbor, Climate and Space Sciences and Engineering, Ann Arbor, MI, United States
Monica M Arienzo, Desert Research Institute, Reno, United States and Joe McConnell, Desert Research Institute, Division of Hydrologic Science, Reno, United States
Natalie Marie Kehrwald1, Piero Zennaro2, McKenzie Skiles3 and Carlo Barbante2, (1)USGS-GECSC, Geosciences and Environmental Change Science Center, Denver, United States, (2)Ca' Foscari University, Department of Environmental Sciences, Informatics and Statistics, Venice, Italy, (3)NASA Jet Propulsion Laboratory, Pasadena, CA, United States