J. L. Pinedo, F. Mireles-García, C. Rios, V. M. Garcia-Saldivar, J. I. Dávila-Rangel, Jose Roberto Espinosa
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引用次数: 4
Abstract
Total Ozone Mapping Spectrometer (TOMS) and Ozone Monitoring Instrument OMI Version 8 data, from November 1978 to February 2013, have been used to retrieve the shape and amplitude of the daily mean of the total column ozone (TCO) and their associated dispersion over eleven selected 1°-wide latitude bands. Their inter-annual variation at 44.5° S, 23.5° S, 23.5° N, 44.5° N and 59.5° N shows a quasi-regular periodic behavior. However, Polar Regions exhibit abrupt changes, whereas at the Equator a complex perturbation of periodicity is highlighted, which could be associated to the effect of the quasi-biennial oscillation (QBO). The discrete 1°-wide latitude bands show a stabilization of TCO levels from the late nineties, but they do not display a generalized recovery. Indeed, at the Equator, between 1997 and 2013, a 1.4% per decade decrease in the total column ozone is exhibited, which may be significant given that during the 1987-1994 period the decrease was only of 0.5%. Additionally, the discrete bands reveal the appearance of a perturbation of the inter-annual ozone variations at 59.5o S, in contrast to regular behavior in the Northern Hemisphere and at other latitudes. The perturbation apparently begins in the 1980-1984 time series and is clear and systematic after 1998.
利用总臭氧测绘光谱仪(TOMS)和臭氧监测仪器OMI Version 8 1978年11月至2013年2月的数据,反演了11个1°宽纬度波段的总柱臭氧(TCO)日均值的形状和振幅及其相关弥散。它们在44.5°S、23.5°S、23.5°N、44.5°N和59.5°N的年际变化表现出准规则的周期性特征。然而,极地地区表现出突变,而赤道地区则表现出周期性的复杂扰动,这可能与准两年一次振荡(QBO)的影响有关。离散的1°宽纬度带显示自90年代末以来TCO水平趋于稳定,但并未显示出普遍的恢复。事实上,在赤道,1997年至2013年期间,臭氧柱总量每十年减少1.4%,考虑到1987年至1994年期间仅减少0.5%,这可能是显著的。此外,离散带显示在59.50 S出现了臭氧年际变化的扰动,这与北半球和其他纬度的正常行为形成对比。扰动明显开始于1980-1984年时间序列,1998年以后较为明显和系统。