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首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >An analysis of Polar Ozone and Aerosol Measurement (POAM) II Arctic polar stratospheric cloud observations, 1993-1996
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An analysis of Polar Ozone and Aerosol Measurement (POAM) II Arctic polar stratospheric cloud observations, 1993-1996

机译:极地臭氧和气溶胶测量(POAM)II北极极地平流层云观测的分析,1993-1996年

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摘要

The Polar Ozone and Aerosol Measurement (POAM) II instrument made numerous observations of polar stratospheric clouds (PSCs) in the northern hemisphere winters of 1993/1994 through 1995/1996. An updated POAM II PSC detection algorithm, described herein, is applied to POAM II 1060 nm aerosol extinction profiles to distinguish PSCs from noncloud measurements. The impact of the updated algorithm on previously published Antarctic PSC statistics is discussed. Operating sporadically in the 1993/1994 PSC season (defined as November through April), but continuously in the following two winters, POAM II made approximately 340 PSC profile measurements. We analyze the POAM II PSC observations with respect to polar vortex location, temperature, longitude, time, and altitude. Daily PSC probability (defined as the number of PSC profiles inside the polar vortex relative to the number of all profiles located inside the vortex) exceeds 60% during the most intense PSC episodes. There is considerable year-to-year variability in PSC probability, preferred location, and timing of onset and final appearance. The POAM II data also reveal interannual differences in the seasonal change of PSC altitude. Certain observations of opaque clouds are used to infer Type II PSCs. The pattern of observed PSCs is discussed with respect to recent studies of Arctic ozone loss.
机译:极地臭氧和气溶胶测量(POAM)II仪器对1993/1994年至1995/1996年北半球冬季的极地平流层云(PSC)进行了多次观测。本文所述的更新的POAM II PSC检测算法适用于POAM II 1060 nm气溶胶消光曲线,以区分PSC与非云测量。讨论了更新的算法对以前发布的南极PSC统计数据的影响。 POAM II在1993/1994 PSC季节(定义为11月至4月)中偶尔运行,但在随后的两个冬季中连续运行,POAM II进行了大约340 PSC剖面测量。我们分析POAM II PSC的极涡位置,温度,经度,时间和高度。在最强烈的PSC发作期间,每日PSC概率(定义为极涡内的PSC轮廓数量相对于位于涡内的所有轮廓数量)超过60%。 PSC机率,首选位置以及发病和最终出现​​的时间逐年变化很大。 POAM II数据还揭示了PSC高度季节性变化的年际差异。不透明云的某些观察结果可用于推断II型PSC。关于北极臭氧损失的最新研究讨论了观察到的PSC的模式。

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