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中国沙漠 ›› 2010, Vol. 30 ›› Issue (3): 691-698.

• 天气与气候 • 上一篇    下一篇

绿化对冬季山谷城市边界层结构影响的数值模拟研究

杨胜朋1,2,3, 吕世华3, 陈玉春3, 奥银焕3, 余 晔3   

  1. 1.气象灾害省部共建教育部重点实验室, 江苏 南京 210044; 2.南京信息工程大学 大气科学学院, 江苏 南京 210044; 3.中国科学院 寒区旱区环境与工程研究所 西部气候环境与灾害实验室, 甘肃 兰州 730000
  • 收稿日期:2009-09-26 修回日期:2009-12-22 出版日期:2010-05-20 发布日期:2010-05-20

Simulation of Afforestation Effect on Urban Boundary Layer Structure of Valley City in Winter

YANG Sheng-peng1,2,3, L Shi-hua3, CHEN Yu-chun3, AO Yin-huan3, Y Ye3   

  1. 1.Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing 210044, China; 2.School of Atmospheric Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China; 3.Laboratory for Climate Environment and Disasters of Western China, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
  • Received:2009-09-26 Revised:2009-12-22 Online:2010-05-20 Published:2010-05-20

摘要: 利用RAMS模式模拟了兰州南北两山绿化对冬季兰州城市边界层结构的影响。结果表明:两山绿化改变了近地面的温度场和风场,从日平均温度来看,绿化在兰州冬季表现为明显的增温效应;从风场来看,白天14:00南山的谷风环流增强,北山变化不明显;晚上02:00北山的山风环流明显增强,南山则出现相反的情况;绿化改变了地表能量平衡,绿化后由于地表反照率的减小,使得到达地面净辐射增加,增加的净辐射其中一部分以感热的形式来加热大气;绿化后地气之间的湍流交换增强,增加了大气不稳定度,减弱了白天城市上空的悬浮逆温;本文还讨论了不同绿化布局对白天悬浮逆温的影响。

关键词: 绿化, 城市边界层结构, 数值模拟, 地表通量

Abstract: The impact of afforestation in the mountains in the north and south of Lanzhou city on urban boundary layer structure in winter is simulated by using RAMS(Regional Atmospheric Modeling System). The numerical simulation results show that afforestation changes the temperature and wind fields in the surface layer. In terms of daily mean temperature field, afforestation exhibits an obviously heating effect to Lanzhou city. According to the wind field, the anabatic wind was strengthened over the south mountains at 14:00 BT(Beijing Time). However, the katabatic wind was strengthened over the north mountains at 02:00 BT. With regard to the energy budget in the winter, the amount of net solar radiation and sensible heat flux is higher on afforestated soil than that on bare soil in permafrost area in winter. The increase of forests can increase the turbulent energy in daytime, and this impact could be transported to the upper atmosphere and results in a weaker elevated temperature inversion. The effect of different greenbelts on the elevated temperature inversion in daytime is also discussed in this paper.

Key words: afforestation, urban boundary layer structure, numerical simulation, surface energy budget

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