Melting of H 2 SO 4 ⋅4H 2 O Particles upon Cooling: Implications for Polar Stratospheric Clouds

Author:

Koop Thomas1,Carslaw Kenneth S.1

Affiliation:

1. Max Planck Institute for Chemistry, Postfach 3060, 55020 Mainz, Germany.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference19 articles.

1. ADRIANI A, J GEOPHYS RES 100, 25977 (1995).

2. STRATOSPHERIC AEROSOL GROWTH AND HNO3 GAS-PHASE DEPLETION FROM COUPLED HNO3 AND WATER-UPTAKE BY LIQUID PARTICLES;CARSLAW K.S.;GEOPHYSICAL RESEARCH LETTERS,1994

3. A THERMODYNAMIC MODEL OF THE SYSTEM HCL-HNO3-H2SO4-H2O, INCLUDING SOLUBILITIES OF HBR, FROM LESS-THAN-200 TO 328 K;CARSLAW K.S.;JOURNAL OF PHYSICAL CHEMISTRY,1995

4. ANALYSIS OF THE PHYSICAL STATE OF ONE ARCTIC POLAR STRATOSPHERIC CLOUD BASED ON OBSERVATIONS;DRDLA K;GEOPHYSICAL RESEARCH LETTERS,1994

5. PHASE EQUILIBRIA OF THE SYSTEM SULFUR TRIOXIDE-WATER;GABLE C.M.;JOURNAL OF THE AMERICAN CHEMICAL SOCIETY,1950

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