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Impact of inland water body changes from 1965 to 2008 on local climate and environment of Wuhan, China

机译:1965年至2008年内陆水体变化对武汉市局部气候和环境的影响

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Water areas have affected the diurnal temperature difference, which block the cooling process at night. But meanwhile the reduction of water bodies can significant affect suburbs climate as temperature increased. That increasing causes the expansion of heat circle, which obstruct the heat dissipation in the centre of urban. As a result, heat accumulated inside urban and the local environment gets hotter and hotter after years. Besides temperature, Water areas change has also affected the wind velocity. And the maximum change can reach to 4.65 ms~(-1). Further research will be done in the accumulation of years' effect in order to get a dynamic effect of process.
机译:水域影响了昼夜温差,从而阻碍了夜间的降温过程。但是与此同时,随着温度的升高,水体的减少会严重影响郊区的气候。这种增加导致热圈的扩大,从而阻碍了城市中心的散热。结果,数年后,城市和当地环境中积累的热量变得越来越热。除温度外,水域变化也影响了风速。最大变化可以达到4.65ms〜(-1)。为了获得过程的动态效果,将对多年效果的累积进行进一步的研究。

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