ANOMALOUS ANTARCTIC OZONE DURING 1992 - EVIDENCE FOR PINATUBO VOLCANIC AEROSOL EFFECTS

被引:65
作者
HOFMANN, DJ [1 ]
OLTMANS, SJ [1 ]
机构
[1] NOAA, CLIMATE MONITORING & DIAGNOST LAB, 325 BROADWAY, BOULDER, CO 80303 USA
关键词
D O I
10.1029/93JD02092
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Unusual stratospheric ozone levels were observed in the Antarctic stratosphere in 1992. The rate of ozone decrease during formation of the springtime ozone hole and the severity of ozone loss in the lower stratosphere were greater in 1992 as compared to previous years. Total ozone reached an all time low of about 105 Dobson units on October 11 at South Pole Station. On this day, the balloon-borne instrument encountered an apparent ozone void between altitudes of 14 and 18 km. Ozone profiles showed evidence of unusual ozone depletion in autumn, before polar stratospheric cloud existence temperatures were reached. Satellite measurements indicated that the 1992 ozone hole was about 25% larger in geographical extent than in previous years. The possible effects of the eruption of the Pinatubo volcano in the Philippine Islands in 1991 are investigated, and it is concluded that the sulfuric acid droplets, which formed in the stratosphere following the eruption and were trapped in the south polar vortex, are the most likely source of the anomalous Antarctic ozone depletion in 1992.
引用
收藏
页码:18555 / 18561
页数:7
相关论文
共 13 条
[1]   MOUNT-PINATUBO AEROSOLS, CHLOROFLUOROCARBONS, AND OZONE DEPLETION [J].
BRASSEUR, G ;
GRANIER, C .
SCIENCE, 1992, 257 (5074) :1239-1242
[2]   VOLCANIC AEROSOL LAYERS OBSERVED BY LIDAR AT SOUTH-POLE, SEPTEMBER 1991 JUNE 1992 [J].
CACCIANI, M ;
DIGIROLAMO, P ;
DISARRA, A ;
FIOCCO, G ;
FUA, D .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (09) :807-810
[3]   VOLCANIC AEROSOL AND OZONE DEPLETION WITHIN THE ANTARCTIC POLAR VORTEX DURING THE AUSTRAL SPRING OF 1991 [J].
DESHLER, T ;
ADRIANI, A ;
GOBBI, GP ;
HOFMANN, DJ ;
DIDONFRANCESCO, G ;
JOHNSON, BJ .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (18) :1819-1822
[4]   THE REACTION PROBABILITIES OF CLONO2 AND N2O5 ON 40-PERCENT TO 75-PERCENT SULFURIC-ACID-SOLUTIONS [J].
HANSON, DR ;
RAVISHANKARA, AR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D9) :17307-17314
[5]   THE EFFECT OF STRATOSPHERIC WATER-VAPOR ON THE HETEROGENEOUS REACTION-RATE OF CLONO2 AND H2O FOR SULFURIC-ACID AEROSOL [J].
HOFMANN, DJ ;
OLTMANS, SJ .
GEOPHYSICAL RESEARCH LETTERS, 1992, 19 (22) :2211-2214
[6]   OBSERVATION AND POSSIBLE CAUSES OF NEW OZONE DEPLETION IN ANTARCTICA IN 1991 [J].
HOFMANN, DJ ;
OLTMANS, SJ ;
HARRIS, JM ;
SOLOMON, S ;
DESHLER, T ;
JOHNSON, BJ .
NATURE, 1992, 359 (6393) :283-287
[7]   OZONE DESTRUCTION THROUGH HETEROGENEOUS CHEMISTRY FOLLOWING THE ERUPTION OF EL CHICHON [J].
HOFMANN, DJ ;
SOLOMON, S .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1989, 94 (D4) :5029-5041
[8]   BALLOON-BORNE MEASUREMENTS OF AEROSOL, CONDENSATION NUCLEI, AND CLOUD PARTICLES IN THE STRATOSPHERE AT MCMURDO STATION, ANTARCTICA, DURING THE SPRING OF 1987 [J].
HOFMANN, DJ ;
ROSEN, JM ;
HARDER, JW ;
HEREFORD, JV .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1989, 94 (D9) :11253-11269
[9]   CATASTROPHIC LOSS OF STRATOSPHERIC OZONE IN DENSE VOLCANIC CLOUDS [J].
PRATHER, M .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D9) :10187-10191
[10]   INCREASED CHLORINE DIOXIDE OVER ANTARCTICA CAUSED BY VOLCANIC AEROSOLS FROM MOUNT-PINATUBO [J].
SOLOMON, S ;
SANDERS, RW ;
GARCIA, RR ;
KEYS, JG .
NATURE, 1993, 363 (6426) :245-248