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USA Dobson spectrophotometer total ozone measurements program: 1962-1992

机译:美国Dobson分光光度计总臭氧测量计划:1962-1992

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A historical overview is presented of Dobson spectrophotometer total ozone observations made by the U.S.A.'s National Oceanic and Atmospheric Administration (NOAA) since the early 1960s. NOAA's contributions in upgrading the quality of total ozone measurements in the global Dobson instrument network, and in providing `ground truth' to satellite ozone observations, are also briefly described. Because ozone trend estimates to within $POM 1% per decade require highest quality data, a program was initiated in 1992 to reprocess the NOAA data with application to the data of final corrections. Trend results for a number of stations are presented and compared with trends derived from satellite instrument ozone measurements. Ozone variations and the downward trend in global ozone of recent years, including the accelerated ozone decrease that began in 1992 and has continued into 1993, are discussed in light of photochemical and dynamical processes that are potentially capable of altering global ozone abundance. Although the Mount Pinatubo eruption of 1991 is suspected of contributing to the most recent decrease in ozone, the mechanisms responsible for the ozone changes observed more than a year after the eruption remain under investigation.
机译:历史概述是由U.S.A.自20世纪60年代初以来的全国海洋和大气管理局(NOAA)制作的ODBSON分光光度计总臭氧观察。 NOAA在升级全球多宇仪器网络中的臭氧测量质量以及向卫星臭氧观测提供“地面真相”的贡献也是简要描述的。由于臭氧趋势估计在$ POM中每十年的1%需要最高质量的数据,因此在1992年开始了一个程序,以便将NOAA数据重新处理到最终更正的数据。提出了许多站的趋势结果,并与卫星仪器臭氧测量源的趋势进行了比较。臭氧变化和近年来,包括加速臭氧减少1992年开始,并一直持续到1993年的全球臭氧的下降趋势中,光有潜在能够改变全球臭氧丰富的光化学和动力学过程进行了讨论。虽然1991年的皮纳图博火山爆发被怀疑有利于臭氧最近减少,负责臭氧变化的机制,观察了一年多后的喷发仍在调查之中。

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