...
首页> 外文期刊>Journal of Applied Meteorology and Climatology >Modeling the Impacts of a Man-Made Lake on the Meteorological Conditions of theSurrounding Areas
【24h】

Modeling the Impacts of a Man-Made Lake on the Meteorological Conditions of theSurrounding Areas

机译:模拟人造湖对周围地区气象条件的影响

获取原文
获取原文并翻译 | 示例
           

摘要

The possible modifications of the surface meteorological conditions due to construction of a small, man-made lake in midlatiludes (surface area of 11.55 km~2 and maximum fetch distance L =5 km) were investigated using the Weather Research and Forecasting (WRF) model (version 3.3). The model was applied to four real typical synoptic situations for which the area of interest was under the influence of a wintertime anticyclone (WA), a wintertime cyclone (WC), a summertime anticyclone (SA), and a summertime cyclone (SC). Each of these four typical synoptic setups was simulated twice—once assuming the present state ("NO-LAKE" experiment) and again assuming the existence of the new lake ("LAKE" experiment). The differences between 36-h average LAKE and NO-LAKE simulation results show noticeable mean changes in the surface temperature and relative humidity as well as a small increase of the mean surface wind speeds in the air above the newly constructed lake. At other portions of the investigated area (distances up to -4L-6L downstream of the new lake), the 36-h mean differences produced by the new lake are below the order of magnitude of accuracy of operational meteorological measurement instruments. In individual hours, however, these differences areoccasionally very high, particularly for cyclonic episodes. In addition, results obtained for SA suggest an existence of a lake circulation cell associated with small differences between the lake and land temperatures (at most up to ~3°-5°C) and consequently, a slight enhancement of slope winds in future (LAKE) conditions.
机译:使用天气研究和预报(WRF)模型研究了在中层裂隙中(面积为11.55 km〜2,最大取水距离L = 5 km)建造的人造小湖可能对地面气象条件造成的影响。 (版本3.3)。该模型应用于四个实际典型天气情境,其关注区域受到冬季反气旋(WA),冬季气旋(WC),夏季反气旋(SA)和夏季气旋(SC)的影响。对这四个典型的天气设置中的每一个都进行了两次模拟-一次假设为当前状态(“无湖”实验),再一次假设存在新的湖泊(“ LAKE”实验)。 36小时平均湖泊和非湖泊模拟结果之间的差异表明,新建湖泊上方的空气中,表面温度和相对湿度的平均变化显着,并且平均表面风速略有增加。在研究区域的其他部分(距离新湖下游-4L-6L的距离),新湖产生的36小时平均差值低于使用中的气象测量仪器的精度等级。但是,在各个小时中,这些差异有时会非常高,尤其是对于气旋发作。此外,从SA获得的结果表明存在一个湖泊环流单元,该湖泊环流单元与湖泊和陆地温度之间的细微差异(最多约3°-5°C)有关,因此,将来坡风会略有增强(湖)条件。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号