THE AIRBORNE ARCTIC STRATOSPHERIC EXPEDITION - PROLOGUE

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

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

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

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

[5] ON THE DEPLETION OF ANTARCTIC OZONE [J]. NATURE, 1986, 321 (6072) : 755 - 758

[6] OBSERVATIONS OF THE NIGHTTIME ABUNDANCE OF OCLO IN THE WINTER STRATOSPHERE ABOVE THULE, GREENLAND [J]. SCIENCE, 1988, 242 (4878) : 550 - 555

[7] CONDENSATION OF HNO3 AND HCL IN THE WINTER POLAR STRATOSPHERES [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1284 - 1287

[8] 1990, IN PRESS OZONE TREND

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

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

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

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

[5] ON THE DEPLETION OF ANTARCTIC OZONE [J]. NATURE, 1986, 321 (6072) : 755 - 758

[6] OBSERVATIONS OF THE NIGHTTIME ABUNDANCE OF OCLO IN THE WINTER STRATOSPHERE ABOVE THULE, GREENLAND [J]. SCIENCE, 1988, 242 (4878) : 550 - 555

[7] CONDENSATION OF HNO3 AND HCL IN THE WINTER POLAR STRATOSPHERES [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (12) : 1284 - 1287

[8] 1990, IN PRESS OZONE TREND