Dual wavelength Raman lidar observations of tropical cirrus clouds during the ALBATROSS campaign 1996

G. Beyerle, H. Schäfer, R. Neuber, P. Rairoux, O. Schrems, I. Mcdermid
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Abstract

Recent model calculations have shown that the extreme dryness of the tropical lower stratosphere can be explained by slow uplift of air masses by large-scale motions leading to the formation of an ubiquitous cirrus cloud layer [1]. We present first results from lidar observations of tropical cirrus clouds above the Atlantic ocean during the ALBATROSS campaign (Atmospheric chemistry and lidar studies above the Atlantic ocean related to ozone and other trace gases in the tropo- and stratosphere) in October-November 1996.
1996年信天翁行动期间热带卷云的双波长拉曼激光雷达观测
最近的模式计算表明,热带平流层下层的极端干燥可以用大规模运动导致气团缓慢上升导致无所不在的卷云层的形成来解释[1]。本文提出1996年10 - 11月“信天翁”(ALBATROSS)项目(对大西洋上空臭氧和其他微量气体在对流层和平流层进行大气化学和激光雷达研究)期间对大西洋上空热带卷云的激光雷达观测的初步结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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