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Lidar observations of elevated temperatures in bright chemiluminescent meteor trails during the 1998 Leonid shower

机译:激光雷达观测1998年狮子座阵雨期间明亮的化学发光流星迹中高温的现象

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Seven persistent trails associated with bright fireballs were probed with a steerable Na wind/temperature lidar at Starfire Optical Range, NM during the 17/18 Nov peak of the 1998 Leonid meteor shower. These chemiluminescence trails were especially rich in Na. The average Na abundance within the trails was 52% of the background Na layer abundance, which suggests that the corresponding masses of the meteors were from 1 g up to 1 kg. CCD images show that the chemiluminescent emissions (including Na and OH) are confined to the walls of a tube, which expands with time by molecular diffusion. Lidar profiles within the trails show that the temperatures are highest at the edges of the tube where the airglow emissions are brightest. Approximately 3 min after ablation, temperatures at the tube walls are 20-50 K warmer than the tube core and background atmosphere. Neither chemical nor frictional heating provides a satisfactory explanation for the observations. [References: 15]
机译:在1998年11月17日至18日狮子座流星雨高峰期间,在新墨西哥州星火光学靶场用可控的Na风/温度激光雷达探测了与明亮火球相关的7条持续路径。这些化学发光迹线尤其富含Na。尾迹中的平均Na丰度为背景Na层丰度的52%,这表明流星的相应质量为1 g至1 kg。 CCD图像显示化学发光(包括Na和OH)被限制在管壁上,该管壁随着时间的推移通过分子扩散而膨胀。轨迹内的激光雷达剖面表明,在烟气排放最亮的管子边缘,温度最高。消融后大约3分钟,管壁处的温度比管芯和背景大气温度高20-50K。化学加热和摩擦加热都不能为观察提供令人满意的解释。 [参考:15]

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