Evidence That Nitric Acid Increases Relative Humidity in Low-Temperature Cirrus Clouds

Author:

Gao R. S.12345,Popp P. J.12345,Fahey D. W.12345,Marcy T. P.12345,Herman R. L.12345,Weinstock E. M.12345,Baumgardner D. G.12345,Garrett T. J.12345,Rosenlof K. H.12345,Thompson T. L.12345,Bui P. T.12345,Ridley B. A.12345,Wofsy S. C.12345,Toon O. B.12345,Tolbert M. A.12345,Kärcher B.12345,Peter Th.12345,Hudson P. K.12345,Weinheimer A. J.12345,Heymsfield A. J.12345

Affiliation:

1. Aeronomy Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305, USA.

2. Cooperative Institute for Research in Environmental Sciences; University of Colorado, Boulder, CO 80309, USA.

3. Laboratory for Atmospheric and Space Physics, Program in Atmospheric and Oceanic Sciences; University of Colorado, Boulder, CO 80309, USA.

4. Department of Chemistry and Biochemistry; University of Colorado, Boulder, CO 80309, USA.

5. NASA Jet Propulsion Laboratory, Pasadena, CA 91109, USA.

Abstract

In situ measurements of the relative humidity with respect to ice (RH i ) and of nitric acid (HNO 3 ) were made in both natural and contrail cirrus clouds in the upper troposphere. At temperatures lower than 202 kelvin, RH i values show a sharp increase to average values of over 130% in both cloud types. These enhanced RH i values are attributed to the presence of a new class of HNO 3 -containing ice particles (Δ-ice). We propose that surface HNO 3 molecules prevent the ice/vapor system from reaching equilibrium by a mechanism similar to that of freezing point depression by antifreeze proteins. Δ-ice represents a new link between global climate and natural and anthropogenic nitrogen oxide emissions. Including Δ-ice in climate models will alter simulated cirrus properties and the distribution of upper tropospheric water vapor.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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