黄河三门峡至花园口区间暴雨的中尺度数值模拟
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A MUNERICAL SIMULATION OF THE RAINSTORM OVER THE BELT FROM THE SAMNEN GORGE TO HUAYUANKOU
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    摘要:

    用有限区域数值模式模拟黄河三门峡至花园口区间及其附近地区七三年七月大暴雨。根据Lavoie的工作,设大气由三层构成:与地面相接的一层为常数通量层,其上为充分混和的混和层,层顶盖有逆温层,最上一层为深厚的稳定层。就混和层说,按基本原始方程取平均值,而对其余两层则作了适当的参数化。就混和层说,考虑到地形影响、地面粗糙度、温度变化、水汽通量及潜热等对初始条件的影响,求基本方程的数值解。按上述模式,模拟结果与实测结果相类似。

    Abstract:

    A limited-area numerical model is used to simulate the "73.7"rainstorm over the belt along the Yellow River from the Sanmen Gorgeto Huayuankou and the adjacent regions. Following Lavoie’s work(1972), a 3-layer atmospheric structure is presented which consists of:i) a constant-flux layer (in contact with the surface); ii) a well-mixedlayer (capped by an inversion) and iii) a deep stratum of stable air.For the well-mixed layer the average is obtained from the governing primitive equations and the other two layers are properly parameterized. The governing equations are solved numerically for mixed layer with consideration of the effect of its initial conditions on the follow-ing factors such as terrain influence, surface roughness, temperature variations, moisture fluxes and the release of latent heat. Results obtained by this model are close to those observed.

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吴和赓,张学军,史金松,1984.黄河三门峡至花园口区间暴雨的中尺度数值模拟[J].大气科学学报,7(1):47-56. Wu Hegen, Zhang Xuejun, Shi Jinsong,1984. A MUNERICAL SIMULATION OF THE RAINSTORM OVER THE BELT FROM THE SAMNEN GORGE TO HUAYUANKOU[J]. Trans Atmos Sci,7(1):47-56.

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