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Rayleigh lidar observations of mesospheric inversion layers at poker flat, Alaska (65 degrees N, 147 degrees W)

机译:阿拉斯加扑克平地中层反演层的瑞利激光雷达观测(北纬65度,北纬147度)

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摘要

Rayleigh lidar measurements of the stratosphere and mesosphere have been made on an ongoing basis over a three-year period at Poker Flat, Alaska (65 degrees N, 147 degrees W). These observations have yielded 27 nightly measurements of the middle atmosphere temperature profile (similar to 40-80 km). These nighttime measurements are distributed between August and April. Mesospheric inversion layers have been observed on five occasions. The average altitude of the inversion layer peak is 60 km, with average amplitude of 18 K. The temperature gradients on the topside of the inversion layers approach the adiabatic lapse rate. The inversion layers do not exhibit the apparent downward phase velocities that are commonly observed at lower latitudes. Furthermore, the inversion layers appear significantly less frequently than at lower latitudes. The observations are discussed in terms of current models and observations at other sites. [References: 30]
机译:在过去三年中,阿拉斯加的扑克平地(北纬65度,西经147度)一直在进行平流层和中间层的瑞利激光雷达测量。这些观测结果对中层大气温度分布(类似于40-80 km)进行了每晚27次测量。这些夜间测量值分布在八月和四月之间。已经有五次观测到中层反演层。反演层峰值的平均高度为60 km,平均振幅为18K。反演层顶部的温度梯度接近绝热流失率。反转层没有表现出通常在较低纬度下观察到的明显的下行速度。此外,反演层的出现频率明显低于低纬度地区。根据其他站点的当前模型和观测值对观测值进行了讨论。 [参考:30]

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