首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Modeling the influence of aerosols on cloud microphysical properties in the east Asia region using a mesoscale model coupled with a bin-based cloud microphysics scheme
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Modeling the influence of aerosols on cloud microphysical properties in the east Asia region using a mesoscale model coupled with a bin-based cloud microphysics scheme

机译:使用中尺度模型结合基于bin的云微物理方案对东亚地区气溶胶对云微物理特性的影响进行建模

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A bin-based microphysics scheme for cloud is implemented into a three-dimensional nonhydrostatic model and off-line coupled with a global aerosol transport model to reproduce realistic and inhomogeneous condensation nuclei (CN) fields. This coupling makes it possible to calculate cloud microphysical properties over a larger area under more realistic environmental conditions. Using the model, nested grid simulations are performed for two precipitation events associated with transitional synoptic-scale forcing during the spring over an area of the East China Sea. The nested grid simulations reproduce the general features of the horizontal distributions of variables such as effective droplet radius derived from satellite data retrieval. Comparison of the relationships among simulated cloud variables with those among satellite-derived variables reveals that the implementation of an inhomogeneous CN field results in a more accurate simulation of the distribution of cloud microphysical properties. Sensitivity tests with respect to CN concentration show that the simulated area and amount of precipitation are slightly affected by the CN concentration. Comparative simulations using bin-based and bulk microphysical schemes indicate that the difference in cloud microphysics has little effect on precipitation except over the areas of elevated pollution (i.e., elevated CN). Comparison with previous reports indicates that the precipitation response to aerosols is dependent on the environmental conditions and the type of the cloud system.
机译:将基于bin的云微物理学方案实施到三维非静水模型中,并与全局气溶胶传输模型脱机,以重现现实的和不均匀的凝聚核(CN)场。这种耦合使得可以在更现实的环境条件下计算较大区域上的云微物理性质。使用该模型,对东海地区春季春季与过渡天气尺度强迫相关的两次降水事件进行了嵌套网格模拟。嵌套网格模拟再现了变量水平分布的一般特征,例如从卫星数据检索中得出的有效液滴半径。比较模拟的云变量与卫星衍生的变量之间的关系,可以发现,非均匀CN场的实施可以更准确地模拟云微物理性质的分布。关于CN浓度的敏感性测试表明,CN浓度对模拟的面积和降水量略有影响。使用基于bin的和整体微物理方案的比较模拟表明,除了在高污染区域(即CN升高)之外,云微物理的差异对降水的影响很小。与先前报告的比较表明,对气溶胶的降水响应取决于环境条件和云系统的类型。

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