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Global isoprene emissions estimated using MEGAN, ECMWF analyses and a detailed canopy environment model

机译:使用MEGAN,ECMWF分析和详细的树冠环境模型估算的全球异戊二烯排放量

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摘要

The global emissions of isoprene are calculated at 0.5° resolutionfor each year between 1995 and 2006, based on the MEGAN (Model of Emissions of Gases andAerosols from Nature) version 2 model (Guenther et al., 2006) and a detailed multi-layer canopy environment model forthe calculation of leaf temperature and visibleradiation fluxes. The calculation is driven by meteorological fields – air temperature,cloud cover, downward solar irradiance, windspeed, volumetric soil moisture in 4 soil layers –provided by analyses of the European Centre for Medium-Range Weather Forecasts (ECMWF).The estimated annual global isoprene emission ranges between 374 Tg (in 1996) and 449 Tg (in1998 and 2005), for an average of ca. 410 Tg/year over the whole period, i.e. about 30% lessthan the standard MEGAN estimate (Guenther et al., 2006). This difference is due, to a large extent, to theimpact of the soil moisture stress factor, which is found here to decrease the global emissionsby more than 20%. In qualitative agreement with past studies, high annual emissions are foundto be generally associated with El Niño events. The emission inventory is evaluated againstflux measurement campaigns at Harvard forest (Massachussets) and Tapajós in Amazonia,showing that the model can capture quite well the short-term variability ofemissions, but that it fails to reproduce the observed seasonal variation at thetropical rainforest site, with largely overestimated wet season fluxes.The comparison of the HCHO vertical columns calculated by a chemistry and transportmodel (CTM) with HCHO distributions retrieved from space provides useful insights on tropicalisoprene emissions. For example, the relatively low emissions calculated over Western Amazonia(compared to the corresponding estimates in the inventory of Guentheret al., 1995)are validated by the excellent agreement found between the CTM and HCHO data over this region.The parameterized impact of the soil moisture stress on isoprene emissions is found toreduce the model/data bias over Australia, but it leads to underestimated emissions near the endof the dry season over subtropical Africa.
机译:基于MEGAN(自然界的气体和气溶胶排放模型)第2版模型(Guenther等,2006)和详细的多层冠层,1995年至2006年之间,每年异戊二烯的全球排放量以0.5°分辨率计算。计算叶片温度和可见辐射通量的环境模型。该计算是由气象领域(空气温度,云量,向下的太阳辐照度,风速,4个土壤层中的土壤含水量)驱动的,该数据由欧洲中型天气预报中心(ECMWF)分析提供。估计的年度全球异戊二烯排放量介于374 Tg(1996年)和449 Tg(1998年和2005年)之间,平均约为。整个期间每年410 Tg,即比标准MEGAN估算值低约30%(Guenther等,2006)。这种差异在很大程度上归因于土壤水分胁迫因子的影响,在这里发现该因子可使全球排放量减少20%以上。与过去的研究在质量上达成一致,发现高年排放量通常与厄尔尼诺事件有关。针对哈佛森林(马萨诸塞州)和亚马逊州塔帕若斯的通量测量活动对排放清单进行了评估,结果表明该模型可以很好地捕获排放的短期变化,但无法再现在热带雨林站点观测到的季节性变化,通过化学和运输模型(CTM)计算的HCHO垂直柱与从太空中检索到的HCHO分布的比较,为热带异戊二烯的排放提供了有用的见解。例如,西部亚马逊地区的相对较低的排放量(与Guentheret等人的清单中的相应估计相比,1995年)通过该地区CTM和HCHO数据之间的出色协议得到了验证。异戊二烯排放的水分压力被发现可以减少澳大利亚的模型/数据偏差,但会导致亚热带非洲旱季末附近的排放被低估。

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