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Ten years of atmospheric methane observations at a high elevation site in Western China

机译:在中国西部高海拔地区进行的十年大气甲烷观测

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In this paper, the continuous (1994-2001) and discrete air sample (1991-2001) measurements of atmospheric CH_4 from the Waliguan Baseline Observatory located in western China (36°17′N, 100°54′E, 3816 masl) are presented and characterized. The CH_4 time series show large episodic events on the order of 100 ppb throughout the year. During spring, a diurnal cycle with average amplitude of 7 ppb and a morning maximum and late afternoon minimum is observed. In winter, a diurnal cycle with average amplitude of 14ppb is observed with an afternoon maximum and morning minimum. Unlike most terrestrial observational sites, no obvious diurnal patterns are present during the summer or autumn. A background data selection procedure was developed based on local horizontal and vertical winds. A selected hourly data set representative of "baseline" conditions was derived with approximately 50% of the valid hourly data. The range of CH_4 mixing ratios, annual means, annual increases and mean annual cycle at Waliguan during the 1992-2001 were derived from discrete and continuous data representative of "baseline" conditions and compared to air samples collected at other Northern Hemisphere sites. The range of CH_4 monthly means of 1746-1822 ppb, average annual means of 1786.7 +- 10.8 ppb and mean annual increase of 4.5 +- 4.2 ppb yr~(-1) at Waliguan were inline with measurements from sites located between 30° and 60°N. There were variations observed in the CH_4 annual increase patterns at Waliguan that were slightly different from the global pattern. The mean CH_4 annual cycle at Waliguan shows an unusual pattern of two gentle peaks in summer and February along with two small valleys in early winter and spring and a mean peak-to-peak amplitude of ~ 11 ppb, much smaller than amplitudes observed at most other mid- and high-northern latitude sites. The Waliguan CH_4 data are strongly influenced by continental Asian CH_4 emissions and provide key information for global atmospheric CH_4 models.
机译:本文通过连续(1994-2001)和离散空气采样(1991-2001)对位于中国西部(36°17′N,100°54′E,3816 masl)的瓦里关基线天文台的大气CH_4进行了测量。介绍和表征。 CH_4时间序列显示全年发生的大型事件约为100 ppb。在春季,观测到一个日平均周期为7 ppb的昼夜周期,一个早晨最大值和一个下午最小值最小值。在冬季,观测到的平均昼夜周期为14ppb,最大下午午后最小。与大多数陆地观测站点不同,夏季或秋季没有明显的昼夜模式。基于局部水平和垂直风,开发了背景数据选择程序。选定的代表“基准”条件的小时数据集将获得约50%的有效小时数据。在1992-2001年期间,瓦里关CH_4的混合比,年平均值,年增长率和年均周期范围是从代表“基线”条件的离散数据和连续数据得出的,并与在北半球其他地点收集的空气样本进行了比较。瓦里关CH_4月平均值范围1746-1822 ppb,年均平均值1786.7 +-10.8 ppb和年均增长率4.5 +-4.2 ppb yr〜(-1)与位于30°和60°N。瓦里关CH_4年增长模式中观察到的变化与全球模式略有不同。瓦里关的CH_4年平均周期显示出异常的模式,在夏季和2月出现两个平缓的峰,在冬季初冬和春季出现两个小谷,平均峰峰幅度为〜11 ppb,远小于最大观测到的幅度。其他中北纬度地点。瓦里关CH_4数据受到亚洲大陆CH_4排放量的强烈影响,并为全球大气CH_4模型提供关键信息。

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