用于传感器测量平流层风的原位声风速计的研制

Song Liang, Hu Xiong, W. Feng, Zhaoai Yan, Qingchen Xu, Tu Cui
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引用次数: 0

摘要

摘要平流层环境对太阳风暴的响应(SENSOR)项目研究太阳风暴对平流层的影响。该项目将于2019年至2022年在中纬度平流层进行一系列飞行实验,采用长时间零压力气球作为平台,携带多种类型的有效载荷。这篇文章描述了一个声学风速计的发展和测试,用于获得沿气球轨迹的原位风测量。开发这种风速计是必要的,因为据作者所知,目前还没有现成的商业产品,能够在平流层的高空气球或其他类似的浮动平台上获得现场风速测量。风速计还配备了温度-压力-湿度测量模块的温度、压力和湿度传感器,该模块继承了为探测气球而开发的无线电探空仪。声波风速仪和其他传感器于2019年9月4日在大柴旦地区(95.37°E, 37.74°N)进行了SENSOR运动的飞行实验。本文介绍了在20公里以上的水平飞行中获得的纬向和经向风速观测结果。这是第一次在这个高度的水平飞行中获得现场风测量。除了风速测量外,上升过程中的温度、压力和相对湿度测量值与四小时前发射的附近无线电探空仪的观测值进行比较。对风力数据的进一步分析将在随后的出版物中发表。声波风速仪在2019年实验中遇到的问题表明,声波风速仪必须在未来的SENSOR运动实验中得到改进。
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Development of an in situ Acoustic Anemometer to Measure Wind in the Stratosphere for SENSOR
Abstract. The Stratospheric Environmental respoNses to Solar stORms (SENSOR) campaign investigates the influence of solar storms on the stratosphere. This campaign employs a long-duration zero-pressure balloon as a platform to carry multiple types of payloads during a series of flight experiments in the mid-latitude stratosphere from 2019 to 2022. This article describes the development and testing of an acoustic anemometer for obtaining in situ wind measurements along the balloon trajectory. Developing this anemometer was necessary, as there is no existing commercial off-the-shelf product, to the authors' knowledge, capable of obtaining in situ wind measurements on a high-altitude balloon or other similar floating platform in the stratosphere. The anemometer is also equipped with temperature, pressure, and humidity sensors from a Temperature-Pressure-Humidity measurement module, inherited from a radiosonde developed for sounding balloons. The acoustic anemometer and other sensors were used in a flight experiment of the SENSOR campaign that took place in the Da chaidan District (95.37° E, 37.74° N) on 4 September 2019. The zonal and meridional wind speed observations, which were obtained during level flight at an altitude exceeding 20 km, are presented. This is the first time that in situ wind measurements were obtained during level flight at this altitude. In addition to wind speed measurements, temperature, pressure, and relative humidity measurements during ascent are compared to observations from a nearby radiosonde launched four hours earlier. Further analysis of the wind data will presented in a subsequent publication. The problems experienced by the acoustic anemometer during the 2019 experiment show that the acoustic anemometer must be improved for future experiments in the SENSOR campaign.
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