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Meteorological and Hydrological Effect of Wind Farm in Arid Areas

机译:干旱地区风电场的气象与水文效应

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Large-scale development of wind farms has not only brought environmental benefits, but it will also affect the local meteorological environment. We chose Zhurihe wind farm, which is located on Sonid Youqi of Inner Mongolia, as our study area. Our observation instrument is the HOBO automatic meteorological station. The observation points are set up in the upwind area, inner wind farm and downwind area. This allows simultaneous observation of land temperature and near-surface air temperature and humidity of 1.5m range of wind farm area and analyze the effect of wind farm on near-surface temperature. The results show that the existence of wind farm would affect temperature and humidity inside and outside of wind farm area. In the daytime (10:00-16:00), there is a cooling and humidifying function in the inner area and downwind area. The relationship of air temperature and land temperature in these three seasons is upwind area>inner wind farm>downwind area. On the contrary, air relative humidity is downwind area>inner wind farm> upwind area, compared with upwind area. This means that the influence of the wind farm on the near surface temperature reduces with the increase in environment air temperature and land temperature while the influence on air relative humidity increases at the same time. The water surface evaporation of 24 hours of the inner wind farm is less than upwind area.
机译:风电场的大规模发展不仅带来了环境效益,而且还会影响当地气象环境。我们选择了Zhurihe风电场,位于内蒙古的Sonid Youqi,作为我们的研究区。我们的观察仪是Hobo自动气象站。观察点位于Upwind区域,内风农场和下行区域。这允许同时观察土地温度和近表面空气温度和湿度为1.5米的风电场区域,并分析风电场对近表面温度的影响。结果表明,风电场的存在会影响风电场内外的温度和湿度。在白天(10:00-16:00)中,内部区域和下行区域存在冷却和加湿功能。这三季空气温度和土地温度的关系是逆风区域>内风农场>下行区域。相反,空气相对湿度是下行区域>内风农场>上风区域,与上风区域相比。这意味着风电场对近表面温度的影响随着环境空气温度和土地温度的增加而减少,而对空气相对湿度的影响同时增加。内风农场24小时的水表面蒸发小于上风区域。

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