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Measurement of Vertical Profiles of CO_2 In The Atmospheric Boundary Layer At A Suburban Site In Summer

机译:夏季郊区近郊大气边界层CO_2垂直剖面的测量

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Knowledge of vertical CO_2 distribution is required for developing 3-D CO_2 transport models and calibration/validation of satellite-borne measurements with ground based remote sensing instruments. In this study, vertical profiles of CO_2 concentration within 0-1000 m were measured using a tethered balloon at a suburban site in Xiamen which is undergoing fast urbanization. The characteristics of CO_2 vertical distribution and the impact from meteorological and anthropogenic factors were investigated using the extended dataset of vertical profiles obtained under both stable and convective boundary-layer conditions during the field campaign. Most of the profiles demonstrated a declining trend of CO_2 concentration with increasing altitude. However, opposite patterns were also observed for some cases that the CO_2 concentration started to increase with altitude above certain heights, where the top of mixing height or inversion layer could be reached according to simultaneous relative humidity and temperature measurements. The correlation of high altitudes and ground level CO_2 concentrations decreased with altitude and show high correlation in the first 300 m with R = 0.783 of 100 m, R = 0.524 of 200 m, R = 0.401 of 300 m (P<0.01). When comparing the vertical profiles obtained at different times during a day, it was found that CO_2 concentration exhibited more obvious diurnal pattern at surface level than at high altitude because of the variation of sources and sinks of CO_2 at ground level. The influence of ground level CO_2 diurnal variation was restricted within the lower 350 m of the atmosphere. The general vertical profiles of CO_2 were fitted to obtain an empirical equation for estimating CO_2 vertical concentration in the lower atmosphere (0-1000m): y = -75.04+1.17e~(-x/28.01), R~2 = 0.59.
机译:要开发3-D CO_2传输模型以及使用地面遥感仪器对卫星测量进行校准/验证,需要具备垂直CO_2分布的知识。在这项研究中,使用系留气球在厦门市郊快速城市化过程中测量了0-1000 m内CO_2浓度的垂直分布。利用野外战役期间在稳定边界层和对流边界层条件下获得的垂直剖面扩展数据集,研究了CO_2垂直分布的特征以及气象和人为因素的影响。大多数剖面表明,随着海拔的升高,CO_2浓度呈下降趋势。但是,在某些情况下,也观察到相反的模式,即CO_2浓度开始随海拔升高而增加,达到一定高度时,根据同时进行的相对湿度和温度测量,可以达到混合高度或反转层的顶部。高海拔地区与地面CO_2浓度的相关性随海拔高度而降低,并且在前300 m中具有高度相关性,R = 0.783 of 100 m,R = 0.524 of 200 m,R = 0.401 of 300 m(P <0.01)。当比较一天中不同时间获得的垂直剖面时,发现由于地面上CO_2的源和汇变化,CO_2浓度在地表水平上表现出比在高海拔处更明显的昼夜模式。地平面CO_2日变化的影响被限制在大气的下部350 m之内。拟合CO_2的一般垂直剖面,以获得估算低层大气(0-1000m)中CO_2垂直浓度的经验方程:y = -75.04 + 1.17e〜(-x / 28.01),R〜2 = 0.59。

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