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基于KF-ETA积云对流参数化方案集合预报试验

Ensemble Experiments Research Based on Mass-Fluxed Cumulus Convective Parameterization of KF-ETA

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采用中尺度数值模式WRF和Kain-Fritsch-ETA积云对流参数化方案(简称KF-ETA方案)对2003年江淮流域一次暴雨过程进行了敏感性分析和集合试验.结果表明,KF-ETA方案中的敏感因子(最小净环境卷入率和积云半径)对预报均有明显的影响,主要体现在各物理变量垂直廓线和次网格对流降水场的分布.基于KF-ETA方案的多成员集合预报,不仅改善了降水的位置和范围、纠正了单一确定性预报中“过干”和“过湿”的随机性偏差,而且也显示预报的不确定性主要集中在地形复杂及强降水的区域.
A Jianghuai rainstorm in 2003 is simulated by WRF model.Furthermore,some sensitive experiments and ensemble studies are done based on Kain-Fritsch-ETA (KF-ETA) scheme.The results reveal that:The minimum net environment entrainment rate and cumulus radius have notable influence on the weather forecast,mainly reflected in the vertical distribution of all kinds of physical variables and grid-scale rainfall distribution.Because of the sensitivity,the location and the scale of the rainfall forecast have been improved through the ensemble mean experiments generated by KF-ETA scheme,as well as the biases of ‘ too dry' and ‘ too moisture' are improved compared with the single random prediction.Meanwhile,some uncertainties are mainly shown in the region with complicated terrain and the rainfall center.

Meso-scale ensemble forecastUncertaintyPhysical perturbation

张曼、闵锦忠、戚友存、杨毅

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南京信息工程大学气象灾害教育部重点实验室,南京210044

南京信息工程大学大气科学学院,南京210044

兰州大学大气科学学院,兰州730000

中尺度集合预报 不确定性 物理过程扰动

国家自然科学基金江苏省高校自然科学重大基础研究项目

40975068,41175092

2014

高原气象
中国科学院寒区旱区环境与工程研究所

高原气象

CSTPCDCSCD北大核心
影响因子:2.193
ISSN:1000-0534
年,卷(期):2014.33(5)
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