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阵风测量技术——从传统风速测量到新的可能性

Wind Gust Measurement Techniques-From Traditional Anemometry to New Possibilities.

作者信息

Suomi Irene, Vihma Timo

机构信息

Meteorological Research, Finnish Meteorological Institute, P.O. Box 503, FI-00101 Helsinki, Finland.

出版信息

Sensors (Basel). 2018 Apr 23;18(4):1300. doi: 10.3390/s18041300.

DOI:10.3390/s18041300
PMID:29690647
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5948875/
Abstract

Information on wind gusts is needed for assessment of wind-induced damage and risks to safety. The measurement of wind gust speed requires a high temporal resolution of the anemometer system, because the gust is defined as a short-duration (seconds) maximum of the fluctuating wind speed. Until the digitalization of wind measurements in the 1990s, the wind gust measurements suffered from limited recording and data processing resources. Therefore, the majority of continuous wind gust records date back at most only by 30 years. Although the response characteristics of anemometer systems are good enough today, the traditional measurement techniques at weather stations based on cup and sonic anemometers are limited to heights and regions where the supporting structures can reach. Therefore, existing measurements are mainly concentrated over densely-populated land areas, whereas from remote locations, such as the marine Arctic, wind gust information is available only from sparse coastal locations. Recent developments of wind gust measurement techniques based on turbulence measurements from research aircraft and from Doppler lidar can potentially provide new information from heights and locations unreachable by traditional measurement techniques. Moreover, fast-developing measurement methods based on Unmanned Aircraft Systems (UASs) may add to better coverage of wind gust measurements in the future. In this paper, we provide an overview of the history and the current status of anemometry from the perspective of wind gusts. Furthermore, a discussion on the potential future directions of wind gust measurement techniques is provided.

摘要

评估风致破坏和安全风险需要阵风信息。阵风速度的测量要求风速仪系统具有较高的时间分辨率,因为阵风被定义为波动风速在短时间(秒级)内的最大值。在20世纪90年代风速测量数字化之前,阵风测量受到记录和数据处理资源的限制。因此,大多数连续的阵风记录最多只能追溯到30年前。尽管如今风速仪系统的响应特性已经足够好,但基于杯式和声波风速仪的气象站传统测量技术仅限于支撑结构能够到达的高度和区域。因此,现有的测量主要集中在人口密集的陆地区域,而在偏远地区,如北冰洋海域,仅在稀疏的沿海地点才能获得阵风信息。基于研究飞机和多普勒激光雷达的湍流测量的阵风测量技术的最新发展,有可能从传统测量技术无法到达的高度和位置提供新的信息。此外,基于无人机系统(UAS)的快速发展的测量方法可能会在未来更好地覆盖阵风测量。在本文中,我们从阵风的角度概述了风速测量的历史和现状。此外,还讨论了阵风测量技术未来可能的发展方向。

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