Abstract
GEOPHYSICAL RESEARCH LETTERS,
VOL. 34,
L24812,
5 PP., 2007
doi:10.1029/2007GL031832
Condensed-phase nitric acid in a tropical subvisible cirrus cloud
Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA
Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA
Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA
Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA
Chemical Sciences Division, NOAA Earth System Research Laboratory, Boulder, Colorado, USA
Atmospheric Research Project, Harvard University, Cambridge, Massachusetts, USA
Atmospheric Research Project, Harvard University, Cambridge, Massachusetts, USA
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
Centro de Ciencias de la Atmosfera, Universidad Nacional Autónoma de México, Mexico City, Mexico
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt, Oberpfaffenhofen, Germany
Department of Engineering, University of Denver, Denver, Colorado, USA
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
NASA Ames Research Center, Moffett Field, California, USA
NASA Ames Research Center, Moffett Field, California, USA
In situ observations in a tropical subvisible cirrus cloud during the Costa Rica Aura Validation Experiment on 2 February 2006 show the presence of condensed-phase nitric acid. The cloud was observed near the tropopause at altitudes of 16.3–17.7 km in an extremely cold (183–191 K) and dry (<5 ppm H2O) air mass. Relative humidities with respect to ice ranged from 150–250% throughout most of the cloud. Optical particle measurements indicate the presence of ice crystals as large as 90 μm in diameter. Condensed HNO3/H2O molar ratios observed in the cloud particles were 1–2 orders of magnitude greater than ratios observed previously in cirrus clouds at similar HNO3 partial pressures. Nitric acid trihydrate saturation ratios were 10 or greater during much of the cloud encounter, indicating that HNO3 may be present in the cloud particles as a stable condensate and not simply physically adsorbed on or trapped in the particles.
Received 27 August 2007; accepted 28 November 2007; published 28 December 2007.
Citation: (2007), Condensed-phase nitric acid in a tropical subvisible cirrus cloud, Geophys. Res. Lett., 34, L24812, doi:10.1029/2007GL031832.
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