LIDAR OBSERVATIONS OF ARCTIC POLAR STRATOSPHERIC CLOUDS, 1988 - SIGNATURE OF SMALL, SOLID PARTICLES ABOVE THE FROST POINT

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

[2] BROWELL EV, 1988, MAY POL OZ WORKSH SN

[3] Cohen A., 1969, J APPL METEOROL, V8, P952, DOI 10.1175/1520-0450(1969)008<0952:AEDOTD>2.0.CO

[4] 2

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

[6] FAHEY DW, 1988, MAY POL OZ WORKSH SN

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

[8] FERRY GV, 1988, MAY POL OZ WORKSH SN

[9] GANDRUD BW, 1988, MAY POL OZ WORKSH SN

[10] Hesstvedt E., 1960, GEOPHYS NORV, V21, P1

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

[2] BROWELL EV, 1988, MAY POL OZ WORKSH SN

[3] Cohen A., 1969, J APPL METEOROL, V8, P952, DOI 10.1175/1520-0450(1969)008<0952:AEDOTD>2.0.CO

[4] 2

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

[6] FAHEY DW, 1988, MAY POL OZ WORKSH SN

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

[8] FERRY GV, 1988, MAY POL OZ WORKSH SN

[9] GANDRUD BW, 1988, MAY POL OZ WORKSH SN

[10] Hesstvedt E., 1960, GEOPHYS NORV, V21, P1