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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Validation of the Improved Limb Atmospheric Spectrometer-II (ILAS-II) Version 1.4 nitrous oxide and methane profiles
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Validation of the Improved Limb Atmospheric Spectrometer-II (ILAS-II) Version 1.4 nitrous oxide and methane profiles

机译:验证改进后的肢体大气Spectrometer-II (ILAS-II)版本1.4一氧化二氮氧化和甲烷的概要文件

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摘要

This study assesses polar stratospheric nitrous oxide (N2O) and methane (CH4) data from the Improved Limb Atmospheric Spectrometer-II (ILAS-II) on board the Advanced Earth Observing Satellite-II (ADEOS-II) retrieved by the Version 1.4 retrieval algorithm. The data were measured between January and October 2003. Vertical profiles of ILAS-II volume mixing ratio (VMR) data are compared with data from two balloon-borne instruments, the Michelson Interferometer for Passive Atmospheric Sounding (MIPAS-B) and the MkIV instrument, as well as with two satellite sensors, the Odin Sub-Millimetre Radiometer (SMR) for N2O and the Halogen Occultation Experiment (HALOE) for CH4. Relative percentage differences between the ILAS-II and balloon/satellite data and their median values are calculated in 10-ppbv-wide bins for N2O (from 0 to 400 ppbv) and in 0.05-ppmv-wide bins for CH4 (from 0 to 2 ppmv) in order to assess systematic differences between the ILAS-II and balloon/satellite data. According to this study, the characteristics of the ILAS-II Version 1.4 N2O and CH4 data differ between hemispheres. For ILAS-II N2O VMR larger than 250 ppbv, the ILAS-II N2O agrees with the balloon/SMR N2O within ±20% in both hemispheres. The ILAS-II N2O in the VMR range from 30–50 to 250 ppbv (corresponding to altitudes of ~17–30 km in the Northern Hemisphere (NH, mainly outside the polar vortex) and ~13–21 km in the Southern Hemisphere (SH, mainly inside the polar vortex) is smaller by ~10–30% than the balloon/SMR N2O. For ILAS-II N2O VMR smaller than 30 ppbv (>~21 km) in the SH, the differences between the ILAS-II and SMR N2O are within ±10 ppbv. For ILAS-II CH4 VMR larger than 1 ppmv (~30 km) and the ILAS-II CH4 for its VMR smaller than 1 ppmv (>~25 km) only in the NH, are abnormally small compared to the balloon/satellite data.
机译:本研究评估极地平流层一氧化二氮氧化(一氧化二氮)和甲烷(CH4)的数据改善肢体大气Spectrometer-II(ILAS-II)先进的地球观测Satellite-II (ADEOS-II)检索的版本1.4检索算法。2003年1月到10月之间。概要文件的ILAS-II体积混合比(VMR)数据与数据从两个气球携带工具,迈克耳逊为被动大气探测干涉仪(MIPAS-B)和MkIV乐器,以及有两个卫星传感器,奥丁一氧化二氮和鼻中隔黏膜下切除术后Sub-Millimetre辐射计()卤素掩蔽实验(CH4 HALOE)项目。相对差异百分比ILAS-II和气球/卫星数据和他们的值计算中位数10-ppbv-wide垃圾箱一氧化二氮(从0到400 ppbv)和0.05 -ppmv-wide垃圾箱CH4(从0到2 ppmv)为了评估系统的差异ILAS-II和气球/卫星数据。这项研究,ILAS-II的特点1.4版本一氧化二氮和甲烷数据之间的不同半球。ppbv, ILAS-II一氧化二氮鼻中隔黏膜下切除术后同意气球/在两个半球一氧化二氮在±20%。一氧化二氮的ppbv VMR范围从30 - 50到250(对应的高度~相当于17 - 30公里北半球(NH,主要是极地之外涡)和~ 13-21公里在南半球(SH,主要在极地漩涡)是小鼻中隔黏膜下切除术后~ 10 - 30%比气球/一氧化二氮。一氧化二氮VMR小于30 ppbv SH(> ~ 21公里),鼻中隔黏膜下切除术后ILAS-II之间的差异和一氧化二氮在±10 ppbv。比1 ppmv( ~ 30公里)ILAS-II CH4的VMR小于1 ppmv (> 25 ~公里)只有在北半球,异常相比较小气球/卫星数据。

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