摘要
对国家气象中心全球预报模式T106L19原有的标准非绝热正规模初始化方案要求外强迫是准静止这一假定进行了修正,将潮汐信号在初始化条件中适当地表达出来并将其从中排除。与三维变分分析SSI的联接对比试验表明,修正潮汐信号后的新方案在消除高频重力波振荡方面与标准初始化方案有同样的效果,但该方案较标准初始化更好地捕捉住了地面气压的半日变化,更接近于未经初始化的分析场。模式7天预报500 hPa高度场与分析场的对比检验表明,新方案的距平相关系数和均方根误差都较原方案有明显的改进。
In this paper, some corrections had been made to the assumption that the forcing is quasi-static, which is the basis of the nonlinear diabatic initialization scheme adopted by a global model T106L19. Thus the tidal signal is expressed and excluded from the initialization scheme. It shows that the new scheme captures the semi-diurnal pressure variation and is closer to the field that is not initialized. Compared with the standard initialization scheme, the anomaly correlation coefficients and RMS of 500 hPa geopotential height simulated under the new scheme have improved significantly.
出处
《热带气象学报》
CSCD
北大核心
2004年第2期145-150,共6页
Journal of Tropical Meteorology
基金
国家"十.五"攻关课题2001BA607B02
中国气象科学研究院7046/2001-9Y-2课题资助
关键词
正规模初始化
潮汐
气压半日变化
initialization
tidal signal
semi-diurnal pressure variation