AIRBORNE LIDAR OBSERVATIONS OF ARCTIC POLAR STRATOSPHERIC CLOUDS - INDICATIONS OF 2 DISTINCT GROWTH-STAGES

[1] LIGHT-SCATTERING BY RANDOMLY ORIENTED SPHEROIDAL PARTICLES [J]. APPLIED OPTICS, 1980, 19 (06): : 962 - 974

[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] CHARACTERISTICS OF POLAR STRATOSPHERIC CLOUDS DURING THE FORMATION OF THE ANTARCTIC OZONE HOLE [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1288 - 1291

[5] KENT GS, 1986, J ATMOS SCI, V43, P2149, DOI 10.1175/1520-0469(1986)043<2149:COAPSC>2.0.CO

[6] 2

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

[8] 2

[9] POLAR STRATOSPHERIC OPTICAL DEPTH OBSERVED BETWEEN 1978 AND 1985 [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D4) : 4297 - 4306

[10] MCCORMICK MP, 1985, J METEOROLOGICAL SOC, V63, P2

[1] LIGHT-SCATTERING BY RANDOMLY ORIENTED SPHEROIDAL PARTICLES [J]. APPLIED OPTICS, 1980, 19 (06): : 962 - 974

[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] CHARACTERISTICS OF POLAR STRATOSPHERIC CLOUDS DURING THE FORMATION OF THE ANTARCTIC OZONE HOLE [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1288 - 1291

[5] KENT GS, 1986, J ATMOS SCI, V43, P2149, DOI 10.1175/1520-0469(1986)043<2149:COAPSC>2.0.CO

[6] 2

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

[8] 2

[9] POLAR STRATOSPHERIC OPTICAL DEPTH OBSERVED BETWEEN 1978 AND 1985 [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1987, 92 (D4) : 4297 - 4306

[10] MCCORMICK MP, 1985, J METEOROLOGICAL SOC, V63, P2