METEOR-3 TOTAL OZONE MAPPING SPECTROMETER OBSERVATIONS OF THE 1993 OZONE HOLE

被引:18
作者
HERMAN, JR
NEWMAN, PA
MCPETERS, R
KRUEGER, AJ
BHARTIA, PK
SEFTOR, CJ
TORRES, O
JAROSS, G
CEBULA, RP
LARKO, D
WELLEMEYER, C
机构
关键词
D O I
10.1029/94JD02316
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The development of the springtime (September-November) Antarctic ozone hole was observed by the Meteor 3/total ozone mapping spectrometer (TOMS) to result in the lowest ozone value, 85 DU (Dobson units) on October 8, 1993, ever measured by TOMS. During late September and early October the region of extremely low ozone values was centered on the geographical pole between 85 degrees S and 90 degrees S. The geographical extent of the ozone hole region, the area within the 220-DU contour, reached a maximum during the first week in October at a near-circular area covering 24 x 10(6) km(2) reaching to the southern tip of South America. This approximately matched the 1992 area record, After the maximum area was reached in early October, the 1993 ozone hole region was significantly larger than during 1992 throughout the remainder of the month of October. The very low ozone values over the Antarctic continent have been confirmed by independent ground-based data. Unlike 1992, the formation of the 1993 Antarctic ozone hole does not coincide with unusually low ozone values observed over most of the globe for the past 2 years. The most recent ozone data from Meteor 3/TOMS show that there has been a recovery at all latitudes from the extraordinarily low values observed during 1992 and part of 1993 after the June 1991 eruption of Mount Pinatubo. Meteor 3/TOMS is described and compared with Nimbus 7/TOMS during the 1991 to May 1993 overlap period. Observations of the 1992 ozone hole are presented from both instruments and are shown to agree within 5 DU.
引用
收藏
页码:2973 / 2983
页数:11
相关论文
共 28 条
[1]  
[Anonymous], 1984, MEM NATL I POLAR RES
[2]  
Cebula R. P., 1988, Journal of Atmospheric and Oceanic Technology, V5, P215, DOI 10.1175/1520-0426(1988)005<0215:COTNSR>2.0.CO
[3]  
2
[4]   LARGE LOSSES OF TOTAL OZONE IN ANTARCTICA REVEAL SEASONAL CLOX/NOX INTERACTION [J].
FARMAN, JC ;
GARDINER, BG ;
SHANKLIN, JD .
NATURE, 1985, 315 (6016) :207-210
[5]   RECORD LOW GLOBAL OZONE IN 1992 [J].
GLEASON, JF ;
BHARTIA, PK ;
HERMAN, JR ;
MCPETERS, R ;
NEWMAN, P ;
STOLARSKI, RS ;
FLYNN, L ;
LABOW, G ;
LARKO, D ;
SEFTOR, C ;
WELLEMEYER, C ;
KOMHYR, WD ;
MILLER, AJ ;
PLANET, W .
SCIENCE, 1993, 260 (5107) :523-526
[6]   A NEW SELF-CALIBRATION METHOD APPLIED TO TOMS AND SBUV BACKSCATTERED ULTRAVIOLET DATA TO DETERMINE LONG-TERM GLOBAL OZONE CHANGE [J].
HERMAN, JR ;
HUDSON, R ;
MCPETERS, R ;
STOLARSKI, R ;
AHMAD, Z ;
GU, XY ;
TAYLOR, S ;
WELLEMEYER, C .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1991, 96 (D4) :7531-7545
[7]   LOW OZONE AMOUNTS DURING 1992-1993 FROM NIMBUS 7 AND METEOR 3 TOTAL OZONE MAPPING SPECTROMETERS [J].
HERMAN, JR ;
LARKO, D .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1994, 99 (D2) :3483-3496
[8]   OZONE DEPLETION AT NORTHERN AND SOUTHERN LATITUDES DERIVED FROM JANUARY 1979 TO DECEMBER 1991 TOTAL OZONE MAPPING SPECTROMETER DATA [J].
HERMAN, JR ;
MCPETERS, R ;
LARKO, D .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1993, 98 (D7) :12783-12793
[9]   ANALYSIS OF THE 8-YEAR TREND IN OZONE DEPLETION FROM EMPIRICAL-MODELS OF SOLAR BACKSCATTERED ULTRAVIOLET INSTRUMENT DEGRADATION [J].
HERMAN, JR ;
HUDSON, RD ;
SERAFINO, G .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D6) :7403-7416
[10]  
HERMAN JR, 1991, J GEOPHYS RES, V96, P17279