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DIURNAL AND SEASONAL VARIATION OF MEASURED ATMOSPHERIC CO_2 AT DEHRADUN DURING 2009

机译:2009年Dehradun在Dehradun的昼夜昼夜变化

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Atmospheric carbon dioxide (CO_2) is the major greenhouse gas. We analysed the diurnal trend and seasonal variations of atmospheric Carbon Dioxide (CO2 ) measured at Dehradun during 2009. The measurements are taken from the Vaisala CO_2 probe installed at the top of the IIRS building. A distinct diurnal cycle with seasonal variations is present in these measurements. Diurnal cycle exhibits a half sinusoidal variation with decreasing phase during sunrise to afternoon and increasing phase during afternoon to sunset. CO_2 mostly remains constant with higher values during the night. The largest negative anomaly with respect to the annual mean varies betwe en +/-20 ppmv with positive anomaly during the night time and negative anomaly during the day time. The cause of such variation could be attributed to the local ecosystem activity. During the day time the sinking of CO_2 through the photosynthesis dominates its release through autotrophic and heterotrophic respiration. On the other hand, photosynthesis has been ceased during the night time and respiration only controls the night variation of CO_2. There exists significant change on the diurnal cycle of CO_2 in different seasons during the year. The maximum rapid decrease in CO_2 concentration in early morning hours is due to photosynthetic activity during the monsoon periods (maximum in August -8ppm). During monsoon period rapid night time increase of CO_2 is observed due to the enhancement of respiration. An inverse relationship exist between model simulated net ecosystem productivity and CO_2 deviations on monthly basis. This diurnal and seasonal variations in situ CO_2 are in confirmation with model simulated results.
机译:大气二氧化碳(CO_2)是主要的温室气体。我们分析了2009年Dehradun在Dehradun测量的大气二氧化碳(CO2)的昼夜趋势和季节变化。测量从安装在IIR建筑物顶部的Vaisala Co_2探针中取出。这些测量中存在具有季节变异的不同昼夜循环。昼夜循环在日出期间与日出期间的阶段降低,下午增加阶段,昼夜循环随着较低的阶段。 CO_2在夜间期间的价值大多数仍然是恒定的。最大的阴性异常相对于年龄在夜间时间和白天的阴性异常期间,在+/-20 ppmv之间变化。这种变异的原因可能归因于当地生态系统活动。在白天,通过光合作用的CO_2的下沉占据通过自养和异养呼吸释放。另一方面,光合作用在夜间时间停止,呼吸只能控制CO_2的夜间变化。在年内不同季节的CO_2昼夜周期存在重大变化。暂存清晨的CO_2浓度的最大迅速降低是由于季风期间的光合活动(8月-8PPM最多)。在季风期间,由于呼吸的增强,观察到CO_2的快速夜间增加。在月度模拟网络生态系统生产力和CO_2偏差之间存在反向关系。这种昼夜和季节性变化在原位CO_2中是以模拟模拟结果的确认。

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