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Stratospheric Aerosol Dynamics over Kamchatka and Its Association with Geophysical Processes

机译:堪察加半岛上的平流层气溶胶动力学及其与地球物理过程的关系

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The dynamics of aerosol layers in comparison with geomagnetic and ionospheric data has been studied based on the nighttime single-frequency lidar sounding of the atmosphere over Kamchatka at altitudes of 10 to 90 km. The relation of the aerosol density to solar, magnetic, and ionospheric activity has been studied, and the stratospheric aerosol formation mechanisms have been considered. It has been indicated that variations in the aerosol density correlate with radiowave absorption, perturbations of the ionospheric parameters, and geomagnetic characteristics. The spatial and time scales of aerosol layers have been estimated. The role of stratospheric aerosol as an indicator of geophysical processes is discussed.
机译:根据地磁在堪察加半岛10至90 km的夜间单频激光雷达探测,研究了与地磁和电离层数据相比的气溶胶层动力学。已经研究了气溶胶密度与太阳,磁和电离层活动的关系,并考虑了平流层气溶胶的形成机理。已经表明,气溶胶密度的变化与无线电波吸收,电离层参数的扰动以及地磁特征有关。已经估计了气溶胶层的空间和时间尺度。讨论了平流层气溶胶作为地球物理过程指示剂的作用。

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