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河北省中南部对流层CH4时空分布特征的飞机探测研究
引用本文:杨洋,董晓波,麦榕,吕峰,王梧熠,孙啸申,王晓青,朱海鹏.河北省中南部对流层CH4时空分布特征的飞机探测研究[J].中国环境科学,2019,39(11):4604-4610.
作者姓名:杨洋  董晓波  麦榕  吕峰  王梧熠  孙啸申  王晓青  朱海鹏
作者单位:1. 河北省气象与生态环境重点实验室, 河北 石家庄 050021;2. 河北省人工影响天气办公室, 河北 石家庄 050021
基金项目:科技部国家重点研发计划(2017YFB0504000);国家自然科学基金资助项目(41730103)
摘    要:为研究河北省中南部对流层内CH4时空分布特征,2018年6~7月利用空中国王350飞机搭载高精度CH4分析仪和相关辅助设备,对河北中南部城市上空(600~5500m)CH4浓度进行飞机探测.探测期间共飞行4架次,取得7组CH4浓度垂直廓线数据.结果表明:探测期间CH4浓度最小值为1884×10-9,最大值为2038×10-9,多架次垂直方向上平均浓度为(1915±90)×10-9.不同探测架次CH4浓度随高度变化趋势有较好的一致性,随高度增加,均出现先增大后减小,后稳定不变的趋势,且在混合层顶以下(约1000m)存在明显分界线.1000m以下,同高度层CH4浓度变化较大,不同架次间浓度相差最大值达124×10-9,同一架次CH4浓度的垂直梯度变化受大气层结影响明显,位温垂直梯度接近零时,CH4浓度的垂直梯度变化不明显.1000m以上,CH4浓度垂直随高度增加呈指数减小,同高度层CH4浓度变化较小,变化偏差在平均值的5%以内,4000m以上,同高度层CH4浓度振幅最小,差值<15×10-9,此时浓度可代表该区域背景大气的平均浓度.石家庄上空同高度层CH4浓度白天整体大于夜间,随高度降低差值变大,说明石家庄白天CH4排放源强度大于夜间.

关 键 词:河北省中南部  对流层  甲烷浓度  时空分布  飞机探测  
收稿时间:2019-04-15

Temporal and spatial distribution of tropospheric CH4 based on aircraft observation in central and southern Hebei Province
YANG Yang,DONG Xiao-bo,MAI Rong,Lü Feng,WANG Wu-yi,SUN Xiao-shen,WANG Xiao-qing,ZHU Hai-peng.Temporal and spatial distribution of tropospheric CH4 based on aircraft observation in central and southern Hebei Province[J].China Environmental Science,2019,39(11):4604-4610.
Authors:YANG Yang  DONG Xiao-bo  MAI Rong  Lü Feng  WANG Wu-yi  SUN Xiao-shen  WANG Xiao-qing  ZHU Hai-peng
Institution:1. Key Laboratory of Meteorology and Ecological Environment of Hebei Province, Shijiazhuang 050021, China;2. Weather Modification Office of Hebei Province, Shijiazhuang 050021, China
Abstract:Aiming to characterize the spatial and temporal distribution of tropospheric CH4 in central and southern Hebei province, CH4 analyzer and associated auxiliary equipment with high precision were mounted on the King-Air 350 and used to acquire the concentration of CH4 over central and southern Hebei province (600m~5500m) during June and July in 2018. Seven sets of vertical profiles were obtained by four flights for CH4 concentration during the observation period, which was the first time in our country. Results showed that the maximum and minimum concentration of CH4 were 2038×10-9 and 1884×10-9, respectively, and the average concentration of CH4 was (1915±90)×10-9. The vertical profiles of CH4 concentration of different flights were in good agreement with the increase of altitude. The CH4 concentration first increased, then decreased, and after that remained almost constant. A clear dividing line was found under the top of the mixed layer (about 1000m). Concentration of CH4 at the same level varied greatly blow this line, and the maximum difference between different flights was 124×10-9. The vertical gradient of CH4 concentration at the same flight was significantly affected by atmospheric junction. The change of vertical gradient of CH4 concentration was not obvious when the vertical gradient of potential temperature was near zero. Above 1000m, the CH4 concentration decreased exponentially with the increase of vertical height. At the same height level, a small change of CH4 concentration was found as the variation deviation was within 5% of the average value. The CH4 concentration at the same height level had the smallest amplitude and the difference value was less than 15×10-9. The CH4 concentration in the same height layer over Shijiazhuang was larger during the daytime than at night, and the difference grew larger with the decrease of height, indicating that the CH4 emission source intensity in Shijiazhuang was greater in the day than at night.
Keywords:central and southern Hebei  troposphere  CH4 concentration  spatial and temporal distribution  aircraft observation  
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