Research Article
Numerical Study of the Effects of Topography and Urbanization on the Local Atmospheric Circulations over the Beijing-Tianjin-Hebei, China
Figure 5
Simulated 10 m wind field and the vertical wind component on the lowest vertical level at 0900 LST and 1900 LST 24 August, 2013; (a) and (c) CNTL and (b) and (d) FLAT. The location of sea breeze inland front can be indicated by the convergence zone with high vertical wind component ().
(a) 0900 |
(b) 0900 |
(c) 1900 |
(d) 1900 |