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Ground-based monitoring of water vapor in the middle atmosphere: the NRL water-vapor millimeter-wave spectrometer

机译:NRL水蒸气毫米波光谱仪对地面大气中的水蒸气进行地面监测

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Abstract: Over the past ten years ground-based mm-wave atmospheric spectroscopy has emerged as a powerful tool for measurements of the vertical profile of water-vapor abundances in the middle atmosphere. The use of masers to provide front-end amplification in previous experiments has, because of their inherent limited rf bandwidth, limited the measurement technique to the mesosphere and upper stratosphere. However, solid-state amplifiers have now emerged with sensitivities nearly as good as those obtained with masers, but with much larger bandwidths. These amplifiers have made it possible to extend the measurement range of this technique into the lower stratosphere. In response to this development, and the need for long- term continuous stratospheric water-vapor measurements, NRL has designed and built a new mm-wave radiometer system specifically designed for making measurements of water vapor in the stratosphere. The instrument, which is based on a high electron mobility transistor (HEMT) front-end amplifier, is described in detail. The data retrieval scheme and the results of an extensive instrument data simulation study are also presented. It is found that knowledge of the tropospheric water-vapor content and profile are important in order to obtain good retrieval accuracy below 30 km.!
机译:摘要:在过去的十年中,基于地面的毫米波大气光谱法已经成为一种强大的工具,可用于测量中层大气中水汽丰度的垂直分布。由于它们固有的有限的射频带宽,在以前的实验中使用激射器来提供前端放大功能已经使测量技术仅限于中层和平流层。但是,现在出现了固态放大器,其灵敏度几乎与微波激射器获得的灵敏度一样好,但是带宽却更大。这些放大器使将这种技术的测量范围扩展到较低的平流层成为可能。为了响应这一发展以及对平流层水汽进行长期连续测量的需要,NRL设计并建造了一种新的毫米波辐射计系统,该系统专门设计用于对平流层中的水汽进行测量。详细介绍了基于高电子迁移率晶体管(HEMT)前端放大器的仪器。还介绍了数据检索方案和广泛的仪器数据模拟研究的结果。发现对流层水汽含量和剖面的知识对于在30 km以下获得良好的取回精度很重要。

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