OVERVIEW OF THE POLAR OZONE ISSUE

[1] THE STABILITY AND PHOTOCHEMISTRY OF DIMERS OF THE CLO RADICAL AND IMPLICATIONS FOR ANTARCTIC OZONE DEPLETION [J]. NATURE, 1988, 332 (6167) : 796 - 800

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

[3] LARGE LOSSES OF TOTAL OZONE IN ANTARCTICA REVEAL SEASONAL CLOX/NOX INTERACTION [J]. NATURE, 1985, 315 (6016) : 207 - 210

[4] BALLOON-BORNE OBSERVATIONS OF THE DEVELOPMENT AND VERTICAL STRUCTURE OF THE ANTARCTIC OZONE HOLE IN 1986 [J]. NATURE, 1987, 326 (6108) : 59 - 62

[5] MCCORMICK MP, 1982, J ATMOS SCI, V39, P1387, DOI 10.1175/1520-0469(1982)039<1387:PSCSBS>2.0.CO

[6] 2

[7] ANTARCTIC O-3 - CHEMICAL MECHANISMS FOR THE SPRING DECREASE [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1296 - 1299

[8] REDUCTIONS OF ANTARCTIC OZONE DUE TO SYNERGISTIC INTERACTIONS OF CHLORINE AND BROMINE [J]. NATURE, 1986, 321 (6072) : 759 - 762

[9] SPRINGTIME STRATOSPHERIC NO2 IN ANTARCTICA [J]. GEOPHYSICAL RESEARCH LETTERS, 1984, 11 (01) : 73 - 75

[10] PRODUCTION OF CL2O2 FROM THE SELF-REACTION OF THE CIO RADICAL [J]. JOURNAL OF PHYSICAL CHEMISTRY, 1987, 91 (02) : 433 - 436

[1] THE STABILITY AND PHOTOCHEMISTRY OF DIMERS OF THE CLO RADICAL AND IMPLICATIONS FOR ANTARCTIC OZONE DEPLETION [J]. NATURE, 1988, 332 (6167) : 796 - 800

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

[3] LARGE LOSSES OF TOTAL OZONE IN ANTARCTICA REVEAL SEASONAL CLOX/NOX INTERACTION [J]. NATURE, 1985, 315 (6016) : 207 - 210

[4] BALLOON-BORNE OBSERVATIONS OF THE DEVELOPMENT AND VERTICAL STRUCTURE OF THE ANTARCTIC OZONE HOLE IN 1986 [J]. NATURE, 1987, 326 (6108) : 59 - 62

[5] MCCORMICK MP, 1982, J ATMOS SCI, V39, P1387, DOI 10.1175/1520-0469(1982)039<1387:PSCSBS>2.0.CO

[6] 2

[7] ANTARCTIC O-3 - CHEMICAL MECHANISMS FOR THE SPRING DECREASE [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1296 - 1299

[8] REDUCTIONS OF ANTARCTIC OZONE DUE TO SYNERGISTIC INTERACTIONS OF CHLORINE AND BROMINE [J]. NATURE, 1986, 321 (6072) : 759 - 762

[9] SPRINGTIME STRATOSPHERIC NO2 IN ANTARCTICA [J]. GEOPHYSICAL RESEARCH LETTERS, 1984, 11 (01) : 73 - 75

[10] PRODUCTION OF CL2O2 FROM THE SELF-REACTION OF THE CIO RADICAL [J]. JOURNAL OF PHYSICAL CHEMISTRY, 1987, 91 (02) : 433 - 436