平流层变化探测网络的新型激光雷达-莫纳罗亚天文台:系统描述

T. D. Walsh, L. O. Lindquist, M. White, Apostolis A. Deslis, I. Mcdermid
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引用次数: 0

摘要

用于平流层臭氧长期测量和可能纳入平流层变化探测网络(NDSC)的差分吸收激光雷达(DIAL)系统的开发[Kurylo和Solomon, 1990]始于1986年喷气推进实验室。JPL桌山设施(TMF, 34.4°N, -117.7°W)的DIAL系统是专门开发的,具有适合NDSC长期测量的特性。1988年2月开始定期测量平流层臭氧浓度曲线,1990年1月开始测量温度,1991年7月开始测量气溶胶。这个系统已经在其他地方得到了充分的描述[McDermid et al ., 1990]。与TMF系统相比,新系统采用了一些新的发展,并介绍了新设计的细节。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New Lidar for the Network for the Detection of Stratospheric Change - Mauna Loa Observatory : System Description
The development of differential absorption lidar (DIAL) systems for long-term measurements of stratospheric ozone and for potential inclusion in the Network for the Detection of Stratospheric Change (NDSC) [Kurylo and Solomon, 1990] began at JPL in 1986. The DIAL system at the JPL Table Mountain Facility (TMF, 34.4° N, -117.7° W) was developed specifically to have the characteristics suitable for long-term measurements as proposed for NDSC. Regular measurements of stratospheric ozone concentration profiles commenced in February 1988, with temperature measurements beginning in January 1990 and aerosol measurements in July 1991. This system has been fully described elsewhere [McDermid et al, 1990]. The new system incorporates some new developments compared to the TMF system and details of the new design are presented.
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