Related Content
Search Google Scholar for:
|
|
Science 23 April 1993: Vol. 260. no. 5107, pp. 523 - 526 DOI: 10.1126/science.260.5107.523
|
|
Articles
Record Low Global Ozone in 1992
J. F. Gleason 1,
P. K. Bhartia 2,
J. R. Herman 2,
R. McPeters 2,
P. Newman 2,
R. S. Stolarski 2,
L. Flynn 3,
G. Labow 4,
D. Larko 4,
C. Seftor 4,
C. Wellemeyer 4,
W. D. Komhyr 5,
A. J. Miller 6, and
W. Planet 7
1 University Space Research Association, and National Aeronautics, and Space Administration, Goddard Space Flight Center (NASA/GSFC), Code 916, Greenbelt, MD 20771
2 Laboratory for Atmospheres, NASA/GSFC, Greenbelt, MD 20771
3 Software Corporation of America, Lanham, MD 20706
4 Hughes-STX Corporation, Lanham, MD 20706
5 Cooperative Institute for Research in Environmental Sciences, University of Colorado and National Oceanographic and Atmospheric Administration (NOAA), Boulder, CO 80303
6 Climate Analysis Center, National Weather Service, NOAA, Camp Springs, MD 20031
7 Satellite Research Laboratory, National Environmental Satellite, Data, and Information Service, NOAA, Camp Springs, MD 20031
The 1992 global average total ozone, measured by the Total Ozone Mapping Spectrometer (TOMS) on the Nimbus-7 satellite, was 2 to 3 percent lower than any earlier year observed by TOMS (1979 to 1991). Ozone amounts were low in a wide range of latitudes in both the Northern and Southern hemispheres, and the largest decreases were in the regions from 10°S to 20°S and 100N to 60°N. Global ozone in 1992 is at least 1.5 percent lower than would be predicted by a statistical model that includes a linear trend and accounts for solar cycle variation and the quasi-biennial oscillation. These results are confirmed by comparisons with data from other ozone monitoring instruments: the SBUV/2 instrument on the NOAA-11 satellite, the TOMS instrument on the Russian Meteor-3 satellite, the World Standard Dobson Instrument 83, and a collection of 22 ground-based Dobson instruments.
Submitted on March 11, 1993
Accepted on March 30, 1993
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
- The 12 900 years BP Laacher See eruption: estimation of volatile yields and simulation of their fate in the plume.
- C. Textor, P. M. Sachs, H.-F. Graf, and T. H. Hansteen (2003)
Geological Society, London, Special Publications
213, 307-328
| Abstract »
| PDF »
- Gene Transfer of a Soluble Receptor of VEGF Inhibits the Growth of Experimental Eyelid Malignant Melanoma.
- S. Shiose, T. Sakamoto, H. Yoshikawa, Y. Hata, Y. Kawano, T. Ishibashi, H. Inomata, K. Takayama, and H. Ueno (2000)
Invest. Ophthalmol. Vis. Sci.
41, 2395-2403
| Abstract »
| Full Text »
- Inhalation devices and propellants.
- (1999)
Can. Med. Assoc. J.
161, s44-50
| Full Text »
- Removal of Stratospheric O3 by Radicals: In Situ Measurements of OH, HO2, NO, NO2, ClO, and BrO.
- P. O. Wennberg, R. C. Cohen, R. M. Stimpfle, J. P. Koplow, J. G. Anderson, R. J. Salawitch, D. W. Fahey, E. L. Woodbridge, E. R. Keim, R. S. Gao, et al. (1994)
Science
266, 398-404
| Abstract »
| PDF »
- Magmatic Vapor Source for Sulfur Dioxide Released During Volcanic Eruptions: Evidence from Mount Pinatubo.
- P. J. Wallace, P. J. Wallace, and T. M. Gerlach (1994)
Science
265, 497-499
| Abstract »
| PDF »
- Sulfate Aerosols and Polar Stratospheric Cloud Formation.
- M. A. Tolbert (1994)
Science
264, 527-528
| PDF »
- Recent Changes in Atmospheric Carbon Monoxide.
- P. C. Novelli, K. A. Masarie, P. P. Tans, and P. M. Lang (1994)
Science
263, 1587-1590
| Abstract »
| PDF »
- Evidence for Large Upward Trends of Ultraviolet-B Radiation Linked to Ozone Depletion.
- J. B. Kerr and C. T. McElroy (1993)
Science
262, 1032-1034
| Abstract »
| PDF »
|
|