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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Investigation of aerosol indirect effects using a cumulus microphysics parameterization in a regional climate model
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Investigation of aerosol indirect effects using a cumulus microphysics parameterization in a regional climate model

机译:在区域气候模型中使用累积微物理参数化研究气溶胶间接效应

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A new Zhang and McFarlane (ZM) cumulus scheme includes a two-moment cloud microphysics parameterization for convective clouds. This allows aerosol effects to be investigated more comprehensively by linking aerosols with microphysical processes in both stratiform clouds that are explicitly resolved and convective clouds that are parameterized in climate models. This new scheme is implemented in the Weather Research and Forecasting model, coupled with the physics and aerosol packages from the Community Atmospheric Model version 5. A case of July 2008 during the East Asian summer monsoon is selected to evaluate the performance of the new ZM and to investigate aerosol effects on monsoon precipitation. The precipitation and radiative fluxes simulated by the new ZM show a better agreement with observations compared to simulations with the original ZM that does not include convective cloud microphysics and aerosol-convective cloud interactions. Detailed analysis suggests that an increase in detrained cloud water and ice mass by the new ZM is responsible for this improvement. Aerosol impacts on cloud properties, precipitation, and radiation are examined by reducing the primary aerosols and anthropogenic emissions to 30% of those in the present (polluted) condition. The simulated surface precipitation is reduced by 9.8% from clean to polluted environment, and the reduction is less significant when microphysics processes are excluded from the cumulus clouds. Cloud fraction is reduced by the increased aerosols due to suppressed convection, except during some heavy precipitation periods when cloud fraction, cloud top height, and rain rate are increased due to enhanced convection.
机译:张和麦克法兰(ZM)的新积云方案包括对流云的两步云微物理参数化。通过将气溶胶与显式分解的层状云和在气候模型中参数化的对流云中的微物理过程联系起来,可以更全面地研究气溶胶的影响。此新方案在“天气研究和预报”模型中实施,并与“社区大气模型”第5版中的物理和气溶胶包结合使用。以2008年7月在东亚夏季风期间的情况为例,来评估新ZM和研究气溶胶对季风降水的影响。与不包含对流云微观物理学和气溶胶-对流云相互作用的原始ZM模拟相比,新ZM模拟的降水和辐射通量与观测值显示出更好的一致性。详细的分析表明,新的ZM减少了云水和冰块的减少是造成这种改善的原因。通过将主要气溶胶和人为排放量减少到当前(污染)条件下的30%来检查气溶胶对云的性质,降水和辐射的影响。从干净的环境到污染的环境,模拟的表面降水减少了9.8%,当从积云中排除微观物理过程时,减少的幅度并不那么显着。由于抑制对流,气溶胶的增加会减少云量,除非在某些强降水期间由于对流增加而使云量,云顶高度和降雨率增加。

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