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鞠永茂, 王亚洲, 王汉杰, 王伟华, 宋帅. 动力数值模式侧边界强迫的改进试验[J]. 气候与环境研究, 2011, 16(2): 149-158. DOI: 10.3878/j.issn.1006-9585.2011.02.04
引用本文: 鞠永茂, 王亚洲, 王汉杰, 王伟华, 宋帅. 动力数值模式侧边界强迫的改进试验[J]. 气候与环境研究, 2011, 16(2): 149-158. DOI: 10.3878/j.issn.1006-9585.2011.02.04
Ju Yongmao, Wang Yazhou, Wang Hanjie, Wang Weihua, Song Shuai. Numerical Experiment of the Lateral Boundary Forcing Improvement of the Nesting Dynamical Model[J]. Climatic and Environmental Research, 2011, 16(2): 149-158. DOI: 10.3878/j.issn.1006-9585.2011.02.04
Citation: Ju Yongmao, Wang Yazhou, Wang Hanjie, Wang Weihua, Song Shuai. Numerical Experiment of the Lateral Boundary Forcing Improvement of the Nesting Dynamical Model[J]. Climatic and Environmental Research, 2011, 16(2): 149-158. DOI: 10.3878/j.issn.1006-9585.2011.02.04

动力数值模式侧边界强迫的改进试验

Numerical Experiment of the Lateral Boundary Forcing Improvement of the Nesting Dynamical Model

  • 摘要: 通过修正嵌套模式侧边界缓冲区温度强迫项的计算方法,使区域气候模式所刻画的温度日变化信息与不同下垫面区域的天气变化规律相符合。进而利用数值模式ASRegCM研究了侧边界缓冲区温度强迫的改进处理对嵌套模式模拟效果的影响,并讨论了其对模拟结果改进的可能机制。数值试验结果表明,该侧边界缓冲区强迫的改进对地面气温和降水距平分布的影响并不明显,但对二者强度的模拟有一定程度的改进,其中地面降水距平量级的改善尤为明显。机理探讨结果认为,模拟效果的改进首先源于侧边界修正处理对原有地面气温波动振幅的放大,其次是侧边界修正处理后地面气温时间演变的模拟中增加了周期为7~10 d的经向和纬向低频波动分量,两者的综合效应抑止了不稳定的对流性降水过程,增加了连续性的非对流性降水,削弱了数值模式中热带和亚热带地区积云对流与非对流云之间的不稳定。

     

    Abstract: The lateral boundary forcing effects in the buffer zones of a nesting modeling system by improving the calculation method of temperature forcing terms are simulated. This new method makes the regional climate model have the ability to describe the daily temperature evolution characteristics that are consistent with the change rules under different underlying surfaces. By using the regional climate model ASRegCM, a numerical experiment is conducted to test the effects of the lateral boundary emulation. Simulation results show that the anomalous intensity of the surface temperature and precipitation is improved with the improvement of temperature calculation in lateral boundary buffer zones, whereas there is no significant change in the distribution pattern of anomalous signs. It also shows that there is more evident improvement in the simulation of precipitation than that of surface temperature though the sensitive test is conducted on temperature only. The improvement in numerical simulation may be concluded into two aspects. One is the amplification effects on wave amplitudes of the surface temperature. The other is the effects of adding the zonal and longitudinal low frequency wave variability component with a 7~10day cycle into the process of lateral buffer emulation. The coeffects restrain the unstable convective precipitation process, and increase the continuous nonconvective precipitation process. And then the instability between cumulus convection and unconvective clouds in tropical and semi tropical zones are weakened during the model simulation.

     

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