HETEROGENEOUS PHYSICOCHEMISTRY OF THE POLAR OZONE HOLE

[1] THE CLOSE RELATION BETWEEN ANTARCTIC TOTAL-OZONE DEPLETION AND COOLING OF THE ANTARCTIC LOW STRATOSPHERE [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1240 - 1243

[2] POLAR STRATOSPHERIC CLOUDS INFERRED FROM SATELLITE DATA [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1256 - 1259

[3] ON THE ATMOSPHERIC PHOTOCHEMISTRY OF NITRIC-ACID [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1986, 91 (D5) : 5477 - 5485

[4] CONTINUING WORLDWIDE INCREASE IN TROPOSPHERIC METHANE, 1978 TO 1987 [J]. SCIENCE, 1988, 239 (4844) : 1129 - 1131

[5] REACTIONS OF NO3 AND N2O5 WITH MOLECULAR-SPECIES OF POSSIBLE ATMOSPHERIC INTEREST [J]. JOURNAL OF PHYSICAL CHEMISTRY, 1987, 91 (23) : 6017 - 6021

[6] CLAVELIN JL, 1979, J CHIM PHYS PCB, V76, P534

[7] COFFEY MT, 1989, J GEOPHYS RES, V94

[8] NITRIC-ACID CLOUD FORMATION IN THE COLD ANTARCTIC STRATOSPHERE - A MAJOR CAUSE FOR THE SPRINGTIME OZONE HOLE [J]. NATURE, 1986, 324 (6098) : 651 - 655

[9] CRUTZEN PJ, 1989, AEROSOLS CLIMATE

[10] HYDROGEN-BOND STUDIES .93. OXONIUM ION IN NITRIC-ACID MONOHYDRATE [J]. ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1975, 31 (MAY15): : 1486 - 1489

[1] THE CLOSE RELATION BETWEEN ANTARCTIC TOTAL-OZONE DEPLETION AND COOLING OF THE ANTARCTIC LOW STRATOSPHERE [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1240 - 1243

[2] POLAR STRATOSPHERIC CLOUDS INFERRED FROM SATELLITE DATA [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1256 - 1259

[3] ON THE ATMOSPHERIC PHOTOCHEMISTRY OF NITRIC-ACID [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1986, 91 (D5) : 5477 - 5485

[4] CONTINUING WORLDWIDE INCREASE IN TROPOSPHERIC METHANE, 1978 TO 1987 [J]. SCIENCE, 1988, 239 (4844) : 1129 - 1131

[5] REACTIONS OF NO3 AND N2O5 WITH MOLECULAR-SPECIES OF POSSIBLE ATMOSPHERIC INTEREST [J]. JOURNAL OF PHYSICAL CHEMISTRY, 1987, 91 (23) : 6017 - 6021

[6] CLAVELIN JL, 1979, J CHIM PHYS PCB, V76, P534

[7] COFFEY MT, 1989, J GEOPHYS RES, V94

[8] NITRIC-ACID CLOUD FORMATION IN THE COLD ANTARCTIC STRATOSPHERE - A MAJOR CAUSE FOR THE SPRINGTIME OZONE HOLE [J]. NATURE, 1986, 324 (6098) : 651 - 655

[9] CRUTZEN PJ, 1989, AEROSOLS CLIMATE

[10] HYDROGEN-BOND STUDIES .93. OXONIUM ION IN NITRIC-ACID MONOHYDRATE [J]. ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE, 1975, 31 (MAY15): : 1486 - 1489