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Significant decline of mesospheric water vapor at the NDACC site near Bern in the period 2007 to 2018

机译:2007年至2018年期间,伯尔尼附近的NDACC站点中层水汽显着下降

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The middle atmospheric water vapor radiometer MIAWARA is located close to Bern in Zimmerwald ( 46.88 sup°/sup N, 7.46 sup°/sup E; 907?m ) and is part of the Network for the Detection of Atmospheric Composition Change (NDACC). Initially built in the year 2002, a major upgrade of the instrument's spectrometer allowed middle atmospheric water vapor to be continuously measured since April 2007. Thenceforward to May 2018, a time series of more than 11 years has been gathered, that makes a first trend estimate possible. For the trend estimation, a robust multilinear parametric trend model has been used. The trend model encompasses a linear term, a solar activity tracker, the El Ni?o–Southern Oscillation (ENSO) index and the Quasi-Biennial Oscillation (QBO) as well as the annual and semi-annual oscillation. In the time period April 2007 to May 2018 we find a significant decline in water vapor by - 0.6 ± 0.2 ppm per decade between 61 and 72?km . Below the stratopause level ( ~48?km ) a smaller reduction of Hsub2/subO of up to - 0.3 ± 0.1 ppm per decade is detected.
机译:中间的大气水蒸气辐射仪MIAWARA位于齐默尔瓦尔德的伯尔尼附近(N为46.88 °,E为7.46 °; 907?m),并且是检测网络的一部分大气成分变化(NDACC)。仪器的光谱仪最初于2002年建成,对仪器进行了重大升级,从2007年4月开始可以连续测量中层大气水蒸气。从现在起到2018年5月,已经收集了超过11年的时间序列,这是对趋势的首次估算可能。对于趋势估计,已经使用了鲁棒的多线性参数趋势模型。趋势模型包括一个线性项,一个太阳活动追踪器,厄尔尼诺-南方涛动(ENSO)指数和准两年一次涛动(QBO)以及年度和半年度振荡。在2007年4月至2018年5月的时间段内,我们发现水汽在61至72公里之间每十年显着下降-0.6±0.2 ppm。在层状顶水平以下(〜48?km)以下,检测到的H 2 O减少幅度较小,最高可达每十倍-0.3±0.1 ppm。

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