利用船载NOAA高分辨率多普勒激光雷达对海洋边界层的24小时观测

V. Wulfmeyer, T. Janjić
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引用次数: 33

摘要

摘要利用NOAA高分辨率多普勒激光雷达(HRDL)在1999年瑙鲁(Nauru99)活动期间获得的船载观测资料,研究了热带太平洋海洋边界层(MBL)的结构。在中尺度活动较弱的一天,利用HRDL背向散射资料观测了对流MBL高度的日变化。观测到的MBL高度日变化幅度约为250 m。研究了MBL高度与海表温度、潜热通量和感热通量的关系。与海表温度有较好的相关性。与潜热通量的相关性较低,MBL高度与感热通量和浮力通量几乎没有相关性。利用HRDL速度数据的速度-方位显示扫描来测量水平风廓线。MBL顶部多为强风切变。这些结果的比较……
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Twenty-Four-Hour Observations of the Marine Boundary Layer Using Shipborne NOAA High-Resolution Doppler Lidar
Abstract Shipborne observations obtained with the NOAA high-resolution Doppler lidar (HRDL) during the 1999 Nauru (Nauru99) campaign were used to study the structure of the marine boundary layer (MBL) in the tropical Pacific Ocean. During a day with weak mesoscale activity, diurnal variability of the height of the convective MBL was observed using HRDL backscatter data. The observed diurnal variation in the MBL height had an amplitude of about 250 m. Relations between the MBL height and in situ measurements of sea surface temperature as well as latent and sensible heat fluxes were examined. Good correlation was found with the sea surface temperature. The correlation with the latent heat flux was lower, and practically no correlation between the MBL height and the sensible heat and buoyancy fluxes could be detected. Horizontal wind profiles were measured using a velocity–azimuth display scan of HRDL velocity data. Strong wind shear at the top of the MBL was observed in most cases. Comparison of these resul...
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