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First lidar observations of polar mesospheric clouds and Fe temperatures at McMurdo (77.8S, 166.7E), Antarctica

机译:南极麦克默多(77.8S,166.7E)极地中层云和铁温度的首次激光雷达观测

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We report the first lidar observations of polar mesospheric clouds (PMCs) and temperatures made with an Fe Boltzmann lidar at McMurdo, Antarctica in summer 2010-2011. Eighty-five hours of PMCs were observed between 21 Dec 2010 and 15 Feb 2011, giving an overall occurrence frequency of 29.9%. The mean PMC centroid altitude is 84.59 0.17 km, confirming previous reports that clouds in the Southern Hemisphere are ~1 km higher than in the North. By combining the McMurdo (77.8S) observations with those obtained at the South Pole (90S) and Rothera (67.5S), we find that the mean PMC altitude increases with increasing latitude with a statistically significant ascending rate of 40 3 m/deg. A negative correlation is found between the daily-mean temperatures at 90 km and PMC brightness. The observations provide direct evidence that the cold phase of wave-induced temperature oscillations facilitates PMC formation and Fe depletion, supporting previous modeling results.
机译:我们报告了2010-2011年夏季在南极麦克默多用Fe Boltzmann激光雷达对极地中层云(PMC)和温度进行的首次激光雷达观测。在2010年12月21日至2011年2月15日期间,观察到85个小时的PMC,总发生频率为29.9%。 PMC的平均质心高度为84.59 0.17 km,这证实了先前的报道,南半球的云比北高约1 km。通过将麦克默多(77.8S)观测值与南极(90S)和罗瑟拉(67.5S)观测值相结合,我们发现PMC的平均高度随纬度的增加而增加,具有统计学上显着的40 3 m / deg的上升速率。在90 km的日平均温度与PMC亮度之间发现负相关。这些发现提供了直接的证据,表明波引起的温度振荡的冷相促进了PMC的形成和铁的消耗,从而支持了先前的建模结果。

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