HNO3 Profiles Obtained During EASOE

F. Murcray, J. R. Starkey, W. Williams, W. Matthews, U. Schmidt, P. Aimedieu, C. Camy‐Peyret
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Abstract

The detection of the Antarctic ozone hole by Farman et all has led to increased interest in obtaining data at high latitudes on the altitude distribution of many of the constituents involved in the photochemistry of the ozone layer. Data concerning the altitude profile of constituents at stratospheric altitudes is generally obtained using instruments flown on large balloons. Launch and recovery of the instrumentation flown on such balloons at remote sites is difficult. In order to reduce these difficulties we have developed small grating spectrometer system which can be flown on small balloons. HNO3is of particular interest in high latitude photochemistry since it is involved in the heterogeneous reactions occurring during the winter. The spectrometer was designed specifically to obtain data on HNO3however the spectral region scanned (8μ to 13μ) includes features due to CH4, N2O, O3, F12 and F11. The system is used to measure the atmospheric spectral emission and its change with altitude as the balloon ascends. The change in spectral radiance with altitude is used to obtain profile data on the constituents of interest.
在EASOE期间获得的HNO3概况
Farman等人对南极臭氧空洞的探测使人们对在高纬度地区获取有关臭氧层光化学中许多成分的高度分布的数据的兴趣增加。关于在平流层高度的成分的高度剖面的数据一般是通过在大气球上飞行的仪器获得的。在偏远地点发射和回收搭载在这种气球上的仪器是很困难的。为了减少这些困难,我们开发了可以在小气球上飞行的小型光栅光谱仪系统。hno3在高纬度光化学中是特别有趣的,因为它参与了冬季发生的非均相反应。该光谱仪是专门为获取hno3数据而设计的,但扫描的光谱区域(8μ ~ 13μ)包含CH4、N2O、O3、F12和F11的特征。该系统用于测量大气光谱发射及其随气球上升高度的变化。光谱辐射随海拔的变化被用来获得感兴趣成分的剖面数据。
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