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Representativeness of single lidar stations for zonally averaged ozone profiles, their trends and attribution to proxies

机译:单一激光雷达站的代表性,以便对齐平均臭氧谱,其趋势和归属于代理

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This paper is focusing on the representativeness of single lidar stations for zonally averaged ozone profile variations over the middle and upper stratosphere. From the lower to the upper stratosphere, ozone profiles from single or grouped lidar stations correlate well with zonal means calculated from the Solar Backscatter Ultraviolet Radiometer (SBUV) satellite overpasses. The best representativeness with significant correlation coefficients is found within ±15° of latitude circles north or south of any lidar station. This paper also includes a multivariate linear regression (MLR) analysis on the relative importance of proxy time series for explaining variations in the vertical ozone profiles. Studied proxies represent variability due to influences outside of the earth system (solar cycle) and within the earth system, i.e. dynamic processes (the Quasi Biennial Oscillation, QBO; the Arctic Oscillation, AO; the Antarctic Oscillation, AAO; the El Ni?o Southern Oscillation, ENSO), those due to volcanic aerosol (aerosol optical depth, AOD), tropopause height changes (including global warming) and those influences due to anthropogenic contributions to atmospheric chemistry (equivalent effective stratospheric chlorine, EESC). Ozone trends are estimated, with and without removal of proxies, from the total available 1980 to 2015 SBUV record. Except for the chemistry related proxy (EESC) and its orthogonal function, the removal of the other proxies does not alter the significance of the estimated long-term trends. At heights above 15hPa an “inflection point” between 1997 and 1999 marks the end of significant negative ozone trends, followed by a recent period between 1998 and 2015 with positive ozone trends. At heights between 15 and 40hPa the pre-1998 negative ozone trends tend to become less significant as we move towards 2015, below which the lower stratosphere ozone decline continues in agreement with findings of recent literature.
机译:本文专注于单一激光雷达站的代表性,以便在中间平流层和上层之间进行分区平均臭氧型变化。从下部到上层层,来自单个或分组的激光雷达站的臭氧型材与来自太阳能反向散射紫外辐射计(SBUV)卫星立交桥计算的区划线相比很好地相关。具有显着相关系数的最佳代表性在任何一个激光器站的纬度圈或南部的纬度圆圈圈内。本文还包括关于代理时间序列的相对重要性的多变量线性回归(MLR)分析,用于解释垂直臭氧谱的变化。所研究的代理代表了由于地球系统(太阳循环)之外和地球系统之外的影响而导致的可变性,即动态过程(准双年生振荡,QBO;北极振荡,AO;南极振荡,AAO; EL NI?o Southern振荡,ENSO),由于火山气溶胶(气溶胶光学深度,AOD),对流层高度的变化(包括全球变暖)和由于人为贡献导致的对大气化学(当量有效的平坦氯,EESES)的影响。估计臭氧趋势,估计,无需删除代理,从1980年至2015年SBUV记录的总可用。除了化学相关代理(EESC)及其正交功能外,还不会改变估计的长期趋势的重要性。在高于15HPA以上的高度,1997年至1999年间“拐点”标志着显着的负面臭氧趋势的结束,其次是1998年至2015年之间的近期,具有积极的臭氧趋势。在15到40HPA之间的高度,1998年前的负面臭氧趋势随着我们迈向2015年的趋势而变得不那么重要,下面较低的平流层臭氧衰落继续与最近文学的结果达成协议。
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