赵鸣. 1995: 赤道带边界层结构的数值研究. 气象学报, (1): 10-18. DOI: 10.11676/qxxb1995.002
引用本文: 赵鸣. 1995: 赤道带边界层结构的数值研究. 气象学报, (1): 10-18. DOI: 10.11676/qxxb1995.002
Zhao Ming. 1995: A NUMERICAL STUDY OF THE PBL STRUCTURE OVER EQUATORIAL ZONE. Acta Meteorologica Sinica, (1): 10-18. DOI: 10.11676/qxxb1995.002
Citation: Zhao Ming. 1995: A NUMERICAL STUDY OF THE PBL STRUCTURE OVER EQUATORIAL ZONE. Acta Meteorologica Sinica, (1): 10-18. DOI: 10.11676/qxxb1995.002

赤道带边界层结构的数值研究

A NUMERICAL STUDY OF THE PBL STRUCTURE OVER EQUATORIAL ZONE

  • 摘要: 在气压随纬度的不同分布条件下,数值求解了二维赤道带大气边界层非线性运动方程组,得到了不同气压分布下赤道带边界层运动特征,显示了平流的重要作用。在赤道带存在低压槽或气压单调随纬度增加而减少的情况下,都得出在赤道附近某纬度有一相应于赤道辐合带(ITCZ)的垂直运动大值集中区域存在,克服了前人用临界纬度机制解释边界层大抽吸速度时略去重要的非线性项的处理上的困难。

     

    Abstract: In this paper, the nonlinear motion equation for the PBL over equatorial zone is solved numerically with different distributions of the pressure with latitude and the motion charactristics of the PBL over the equatorical zone are obtained. The results show the important role played by advection and the solution indicates that corresponding to ITCZ, near the equartor there exists a concentrated zone where the vertical velocity at the top of the PBL is great both when there is a low pressure zone near the equator and the pressure decreases with the increase of latitude monotonically, this overcomes the difficulty of the critical latitude mechanism which neglects the large nonlinear advective terms.

     

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