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MID-LATITUDE NOCTILUCENT CLOUD OBSERVATIONS BY LIDAR

机译:激光雷达中纬线夜光云观测

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Regular zenith-directed Rayleigh lidar soundings at Juliusruh (54.63 degrees N, 13.38 degrees E) in summer 1995 indicated the presence of overhead noctilucent clouds (NLC) during three nights in June. For two of these nights, NLC were also sighted visually near the northern horizon. For one of the lidar-observed NLC events, temperature profiles were obtained immediately prior to the appearance of the NLC. These show at 81 km a strong cooling of about 30 K within two hours. The wind velocity and direction during the NLC events were inferred from daytime common-volume MF radar wind measurements. During the occurrence of the NLCs the interpolated MF radar wind was south-westwards directed with velocities between 9 - 32 m/s. Different from high latitudes, NLCs can be observed by lidar at mid-latitudes in total darkness. Therefore, mid-latitude observations hold the promise to allow a characterisation of NLC particle size distributions and particle densities even with comparatively simple, multi-color lidars. [References: 13]
机译:1995年夏天,在朱利叶斯鲁(北纬54.63度,东经13.38度)进行定期的天顶定向瑞利激光雷达探测,表明6月的三个晚上存在高架夜光云(NLC)。在这两个夜晚中,在北部地平线附近也目睹了NLC。对于激光雷达观测到的NLC事件之一,在NLC出现之前立即获得了温度曲线。这些显示出在两个小时内在81 km处约30 K的强烈冷却。 NLC事件期间的风速和风向是从白天的普通容积MF雷达风测量推算得出的。在NLC发生期间,内插的MF雷达风向西南方向以9-32 m / s的速度定向。与高纬度不同,中低纬度的激光雷达可以在完全黑暗的情况下观察到NLC。因此,即使使用相对简单的多色激光雷达,中纬度观测也有望实现NLC粒度分布和颗粒密度的表征。 [参考:13]

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