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首页> 外文期刊>Atmospheric Measurement Techniques >Simulation study for measurement of horizontal wind profiles in the polar stratosphere and mesosphere using ground-based observations of ozone and carbon monoxide lines in the 230–250?GHz region
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Simulation study for measurement of horizontal wind profiles in the polar stratosphere and mesosphere using ground-based observations of ozone and carbon monoxide lines in the 230–250?GHz region

机译:利用对230-250?GHz区域中臭氧和一氧化碳线的地面观测,对平流层和中间层水平风廓线进行测量的模拟研究

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摘要

Meteorological and atmospheric models are being extended up to 80?km altitude but there are very few observing techniques that can measure stratospheric–mesospheric winds at altitudes between 20 and 80?km to verify model datasets. Here we demonstrate the feasibility of horizontal wind profile measurements using ground-based passive millimetre-wave spectroradiometric observations of ozone lines centred at 231.28, 249.79, and 249.96?GHz. Vertical profiles of horizontal winds are retrieved from forward and inverse modelling simulations of the line-of-sight Doppler-shifted atmospheric emission lines above Halley station (75°37′?S, 26°14′?W), Antarctica. For a radiometer with a system temperature of 1400?K and 30?kHz spectral resolution observing the ozone 231.28?GHz line we estimate that 12?h zonal and meridional wind profiles could be determined over the altitude range 25–74?km in winter, and 28–66?km in summer. Height-dependent measurement uncertainties are in the range 3–8?m?ssup?1/sup and vertical resolution ?~??8–16?km. Under optimum observing conditions at Halley a temporal resolution of 1.5?h for measuring either zonal or meridional winds is possible, reducing to 0.5?h for a radiometer with a 700?K system temperature. Combining observations of the 231.28?GHz ozone line and the 230.54?GHz carbon monoxide line gives additional altitude coverage at 85?±?12?km. The effects of clear-sky seasonal mean winter/summer conditions, zenith angle of the received atmospheric emission, and spectrometer frequency resolution on the altitude coverage, measurement uncertainty, and height and time resolution of the retrieved wind profiles have been determined.
机译:气象和大气模型正在扩展到80 km公里的高度,但是很少有观测技术能够测量20至80 km km高度的平流层-中层风,以验证模型数据集。在这里,我们演示了使用以231.28、249.79和249.96?GHz为中心的臭氧线的地面被动毫米波光谱辐射观测法进行水平风廓线测量的可行性。从南极哈雷站(75°37′?S,26°14′?W)上方视线多普勒频移的大气排放线的正向和逆向模拟模拟中,可以获得水平风的垂直剖面。对于系统温度为1400?K,光谱分辨率为30?kHz的辐射计,观察臭氧231.28?GHz线,我们估计冬季25-74?km的海拔范围内可以确定12?h纬向和经向风廓线,夏季28-66公里。与高度有关的测量不确定度在3–8?m?s ?1 范围内,垂直分辨率在?〜?? 8-16?km。在Halley的最佳观测条件下,用于测量纬向风或子午风的时间分辨率为1.5?h,对于系统温度为700?K的辐射计,其时间分辨率为0.5?h。结合231.28?GHz臭氧线和230.54?GHz一氧化碳线的观测结果,可以得到85?±?12?km的额外高度覆盖。确定了晴空季节平均冬季/夏季条件,接收到的大气排放的天顶角以及光谱仪频率分辨率对海拔覆盖率,测量不确定度以及检索到的风廓线的高度和时间分辨率的影响。

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