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Numerical Study of the Effects of Topography and Urbanization on the Local Atmospheric Circulations over the Beijing-Tianjin-Hebei, China

机译:京津冀地区地形和城市化对当地大气环流影响的数值研究

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The effects of the topography and urbanization on the local atmospheric circulations over the Beijing-Tianjin-Hebei (BTH) region were studied by the weather research and forecasting (WRF) model, as well as the interactions among these local atmospheric circulations. It was found that, in the summer day time, the multiscale thermally induced local atmospheric circulations may exist and interact in the same time over the BTH region; the topography played a role in the strengthening of the sea breeze circulations; after sunset, the inland progress of sea breeze was slowed down by the opposite mountain breeze; when the land breeze circulation dominated the Bohai bay, the mountain breeze circulation can couple with the land breeze circulation to form a large circulation ranging from the coastline to the mountains. And the presence of cities cannot change the general state of the sea-land breeze (SLB) circulation and mountain-valley breeze (MVB) circulation but acted to modify these local circulations slightly. Meanwhile, the development of the urban heat island (UHI) circulation was also strongly influenced by the nearby SLB circulation and MVB circulation.
机译:通过天气研究与预报(WRF)模型以及这些局部大气环流之间的相互作用,研究了地形和城市化对京津冀(BTH)地区局部大气环流的影响。研究发现,在夏季,BTH区域可能同时存在多尺度的热致局部大气环流并同时相互作用。地形在加强海风环流方面发挥了作用。日落之后,海风向内陆的前进被对面的山风放慢了。当陆风环流主导渤海湾时,山风环流可以与陆风环流耦合,形成从海岸线到山脉的大环流。城市的存在并不能改变海陆风(SLB)和山谷风(MVB)环流的总体状态,但是可以稍微改变这些局部环流。同时,城市热岛(UHI)环流的发展也受到附近SLB环流和MVB环流的强烈影响。

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