从拉曼激光雷达观测热带太平洋的大气特性

W. Eichinger, D. Cooper, L. Tellier, Michael A. Osborne
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引用次数: 0

摘要

地面-大气相互作用是一种动力学过程,首次通过机载扫描水汽拉曼激光雷达在四个维度上观察到。直到最近,关键的边界层变量,如水蒸气,都是从浮标、无线电探空仪、船舶或飞机上的点传感器收集的时间序列数据中估计出来的。相比之下,扫描水汽拉曼激光雷达已被用于评估大气边界层(ABL)的空间和时间特征,其分辨率以前是大气研究人员无法获得的。在1993年和1996年的两次海洋实验中,洛斯阿拉莫斯国家实验室(Los Alamos National Laboratory, LANL)小组对热带太平洋的边界层行为进行了详细测量,将海表温度(SST)与边界层高度、潜能通量和海洋表面上方的间歇对流结构联系起来。对这些实验数据的分析有助于集中研究海洋-大气界面内复杂动力学的知识体系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Atmospheric Properties in the Tropical Pacific from Raman Lidar
Surface-atmosphere interactions are dynamical processes that have for the first time been observed in four dimensions by a ship-board scanning water vapor Raman lidar. Until recently, critical boundary layer variables such as water vapor have been estimated from time-series data collected by point sensors on buoys, radiosondes, ships, or aircraft. In contrast, the scanning water vapor Raman lidar has been used to evaluate the spatial as well as temporal characteristics of the atmospheric boundary layer (ABL) with resolution previously unavailable to atmospheric researchers. On two oceanic experiments in 1993 and 1996, the Los Alamos National Laboratory (LANL) team made detailed measurements of boundary layer behavior in the Tropical Pacific, relating sea surface temperature (SST) to boundary layer height, latent energy flux, and intermittent convective structures above the ocean surface. The analysis of the data from these experiments are contributing to the body of knowledge focusing upon the complex dynamics within the ocean-atmosphere interface.
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