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首页> 外文期刊>Atmospheric Measurement Techniques Discussions >Three decades of tropospheric ozone lidar development at Garmisch-Partenkirchen, Germany
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Three decades of tropospheric ozone lidar development at Garmisch-Partenkirchen, Germany

机译:三十年来德国Garmisch-Partenkirchen的TroposhiC臭氧Lidar开发

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Since 1988 two ozone lidar systems have been developed at IMK-IFU (Garmisch-Partenkirchen, Germany). A stationary system, operated at the institute, has yielded about 5000 vertical profiles of ozone from next to the ground to typically 3km above the tropopause and has contributed data for a large number of scientific investigations. A mobile system was successfully operated in a number of field campaigns after its completion in 1996, before it was destroyed in major flooding in May?1999. Both systems combine high data quality with high vertical resolution dynamically varied between 50m in the lower troposphere and 250–500m below the tropopause (stationary system). The stationary system has been gradually upgraded over the years. The noise level of the raw data has reached about ±1×10-6 of the input range of the transient digitizers after minor smoothing. As a consequence, uncertainties in the ozone mixing ratios of 1.5 to 4ppb have been achieved up to about 5km. The performance in the upper troposphere, based on the wavelength pair 292–313nm, varies between 5 and 15ppb depending on the absorption of the 292nm radiation by ozone and the solar background. In summer it is therefore planned to extend the measurement time from 41s to a few minutes in order to improve the performance to a level that will allow us to trust automatic data evaluation. As a result of the time needed for manual refinement the number of measurements per year has been restricted to under 600. For longer time series automatic data acquisition has been used.
机译:自1988年以来,已在IMK-IFU(Garmisch-Partenkirchen,Germany)开发了两种臭氧激光雷达系统。在该研究所运营的固定系统,从地面旁边产生了大约5000个垂直型材,以至于对流博士以上3km,并为大量科学调查提供了贡献。在1996年完成后,移动系统成功运营了一些现场活动,然后在5月份在大量洪水中被摧毁之前?1999年。两种系统将高数据质量与高垂直分辨率相结合,在较低的对流层中动态变化在50米之间,下方250-500米以下(静止系统)。静止系统多年来一直逐渐升级。在轻微平滑后,原始数据的噪声水平达到瞬态数字的输入范围的±1×10-6。因此,臭氧混合比的不确定性已达到约5km的1.5至4ppb。基于波长对292-313nm的上层对流层的性能根据臭氧和太阳能背景的292nm辐射的吸收而变化5至15ppb。因此,在夏季,计划将测量时间从41s扩展到几分钟,以便将性能提高到允许我们信任自动数据评估的水平。由于手动细化所需的时间,每年的测量数量仅限于600岁以下。对于较长时间序列,已使用自动数据采集。

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