Vapor Pressures of Solid Hydrates of Nitric Acid: Implications for Polar Stratospheric Clouds
Author:
Affiliation:
1. Center for Chemical and Environmental Physics, Aerodyne Research, Inc., Billerica, MA 01821
2. Division of Applied Sciences, Harvard University, Cambridge, MA 02138
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
Reference37 articles.
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2. CRUTZEN, P.J., NITRIC-ACID CLOUD FORMATION IN THE COLD ANTARCTIC STRATOSPHERE - A MAJOR CAUSE FOR THE SPRINGTIME OZONE HOLE, NATURE 324: 651 (1986).
3. DYE, J.E., OBSERVED PARTICLE EVOLUTION IN THE POLAR STRATOSPHERIC CLOUD OF JANUARY 24, 1989, GEOPHYSICAL RESEARCH LETTERS 17: 413 (1990).
4. DYE, J.E., PARTICLE-SIZE DISTRIBUTIONS IN ARCTIC POLAR STRATOSPHERIC CLOUDS, GROWTH AND FREEZING OF SULFURIC-ACID DROPLETS, AND IMPLICATIONS FOR CLOUD FORMATION, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 97: 8015 (1992).
5. FAHEY, D.W., INSITU MEASUREMENTS OF TOTAL REACTIVE NITROGEN, TOTAL WATER, AND AEROSOL IN A POLAR STRATOSPHERIC CLOUD IN THE ANTARCTIC, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 94: 11299 (1989).
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