1. 有限区域谱展前后的均方根误差比全球范围的相应值要小2—3位势米，这主要是由于有限区域内纬向格距较小的缘故。
This is principally due to the longitudinal gridlength is shorter for the limited areas than that for the globe.
2. 青藏高原大气边界层内纬向涡旋的形成及其数值模拟研究
A study of numerical simulation of zonal vortex formation in the boundary layer over the Qinghai-Xizang Plateau