首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >AN UNCERTAINTY BUDGET FOR GROUND-BASED FOURIER TRANSFORM INFRARED COLUMN MEASUREMENTS OF HCL, HF, N2O, AND HNO3, DEDUCED FROM RESULTS OF SIDE-BY-SIDE INSTRUMENT INTERCOMPARISONS
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AN UNCERTAINTY BUDGET FOR GROUND-BASED FOURIER TRANSFORM INFRARED COLUMN MEASUREMENTS OF HCL, HF, N2O, AND HNO3, DEDUCED FROM RESULTS OF SIDE-BY-SIDE INSTRUMENT INTERCOMPARISONS

机译:基于仪器相互比较结果得出的HCL,HF,N2O和HNO3的基于地面的傅里叶变换红外柱测量的不确定性预算

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The results of side-by-side instrument intercomparisons of Fourier transform infrared (FTIR) spectrometers at Ny-Alesund, Spitzbergen (79 degrees N, 12 degrees E), during May/June 1995 and at Harestua, Norway (60 degrees N, 10 degrees E), during September/October 1994 are reported. The spectrometers were operated simultaneously recording atmospheric spectra in the midinfrared using the Sun as a source. The differences in vertical columns of HCl, HF, N2O, and HNO3 measured simultaneously by different instruments were as large as 5.8, 7.7, 2.8, and 4.3%, respectively, having mean absolute values 0.5, 1.6, 1.0, and 1.6%, respectively. These results were used to derive la overall uncertainties of 9.7% for HCl, 7.7% for HF, 6.4% for N2O, and 14.3% for HNO3. Separate uncertainties are quoted for the precision of daily column measurements which exclude the contribution due to uncertainty in the line parameters. These are 7.7% for HCl, 5.7% for HF, 4.9% for N2O, and 6.8% for HNO3. These numbers are estimated for the local conditions at the intercomparison sites but will differ from site to site depending on the knowledge of local atmospheric conditions at the time of measurement. [References: 12]
机译:1995年5月/ 6月在Spitzbergen的Ny-Alesund(北纬79度)和挪威的Harestua(北纬60度,10度)的Fourier变换红外(FTIR)光谱仪的并排仪器比对结果据报道,在1994年9月/ 10月。使用太阳作为光源,同时操作光谱仪以记录中红外的大气光谱。用不同仪器同时测量的HCl,HF,N2O和HNO3垂直柱的差异分别大到5.8%,7.7%,2.8%和4.3%,平均绝对值分别为0.5%,1.6%,1.0%和1.6% 。这些结果用于得出HCl的总体不确定度为9.7%,HF为7.7%,N2O为6.4%,HNO3为14.3%。每日色谱柱测量的精确度引用了单独的不确定性,其中不包括线路参数不确定性造成的影响。 HCl为7.7%,HF为5.7%,N2O为4.9%,HNO3为6.8%。这些数字是根据比对地点的当地情况估算的,但根据测量时对当地大气状况的了解,地点之间会有所不同。 [参考:12]

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