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首页> 外文期刊>Journal of Applied Meteorology and Climatology >Urbanization Impacts on the Climate in Europe: Numerical Experiments by the PSU-NCAR Mesoscale Model (MM5)
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Urbanization Impacts on the Climate in Europe: Numerical Experiments by the PSU-NCAR Mesoscale Model (MM5)

机译:城市化进程对欧洲气候的影响:PSU-NCAR中尺度模型(MM5)的数值实验

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摘要

The objective of this study is to investigate the effects of urban land on the climate in Europe on local and regional scales. Effects of urban land cover on the climate are isolated using the fifth-generation Pennsylvania State University–National Center for Atmospheric Research (PSU–NCAR) Mesoscale Model (MM5) with a modified land surface scheme based on the Town Energy Budget model. Two model scenarios represent responses of climate to different states of urbanization in Europe: 1) no urban areas and 2) urban land in the actual state in the beginning of the twenty-first century. By comparing the simulations of these contrasting scenarios, spatial differences in near-surface temperature and precipitation are quantified. Simulated near-surface temperatures and an urban heat island for January and July over a period of 6 yr (2000–05) agree well with corresponding measurements at selected urban areas. The conversion of rural to urban land results in statistically significant changes to precipitation and near-surface temperature over areas of the land cover perturbations. The diurnal temperature range in urbanized regions was reduced on average by 1.26° ± 0.71°C in summer and by 0.73° ± 00.54°C in winter. Inclusion of urban areas results inan increase of urban precipitation in winter (0.09 ± 00.16 mm day~(-1)) and a precipitation reduction in summer (-0.05 ± 0.22 mm day~(-1)).
机译:这项研究的目的是调查城市土地对欧洲气候在局部和区域尺度上的影响。使用第五代宾夕法尼亚州立大学-国家大气研究中心(PSU-NCAR)中尺度模型(MM5),以基于城镇能源预算模型的改良地表方案,隔离了城市土地覆盖对气候的影响。两种模式情景代表了气候对欧洲不同城市化状态的响应:1)无市区; 2)二十一世纪初的实际状态中的城市土地。通过比较这些对比情景的模拟,可以量化近地表温度和降水的空间差异。模拟的近地表温度和6年(2000-05)期间1月和7月的城市热岛与选定城市地区的相应测量结果非常吻合。农村土地向城市土地的转化导致土地覆盖扰动区域的降水和近地表温度发生统计学上的显着变化。夏季,城市地区的日平均温度范围平均降低了1.26°±0.71°C,而冬季则平均降低了0.73°±00.54°C。将城市地区包括在内会导致冬季(0.09±00.16 mm日〜(-1))的城市降水增加,而夏季(-0.05±0.22 mm日〜(-1))的降水减少。

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