高级检索
洪雯, 王毅勇, 聂晓. 湿地下垫面大气边界层温、湿廓线的数值模拟及影响因素分析[J]. 气候与环境研究, 2011, 16(4): 494-504. DOI: 10.3878/j.issn.1006-9585.2011.04.10
引用本文: 洪雯, 王毅勇, 聂晓. 湿地下垫面大气边界层温、湿廓线的数值模拟及影响因素分析[J]. 气候与环境研究, 2011, 16(4): 494-504. DOI: 10.3878/j.issn.1006-9585.2011.04.10
Hong Wen, Wang Yiyong, Nie Xiao. Numerical Simulation of Temperature and Humidity Profiles in Atmospheric Boundary Layer over Wetland and Analysis of Influence Factors[J]. Climatic and Environmental Research, 2011, 16(4): 494-504. DOI: 10.3878/j.issn.1006-9585.2011.04.10
Citation: Hong Wen, Wang Yiyong, Nie Xiao. Numerical Simulation of Temperature and Humidity Profiles in Atmospheric Boundary Layer over Wetland and Analysis of Influence Factors[J]. Climatic and Environmental Research, 2011, 16(4): 494-504. DOI: 10.3878/j.issn.1006-9585.2011.04.10

湿地下垫面大气边界层温、湿廓线的数值模拟及影响因素分析

Numerical Simulation of Temperature and Humidity Profiles in Atmospheric Boundary Layer over Wetland and Analysis of Influence Factors

  • 摘要: 应用大气二维边界层数值模式,对2008年夏季洪河国家级自然保护区沼泽湿地1000 m高度边界层的温度、湿度廓线进行了3次模拟试验,并模拟分析了风速和下垫面粗糙度对湿地边界层温、湿廓线结构的影响。结果表明:(1)大气二维边界层模式可以较好的模拟湿地下垫面边界层的温、湿结构,并且该模式对位温的模拟效果优于比湿;(2)风速和粗糙度是湿地下垫面大气边界层温、湿廓线结构的主要影响因素。60 m以下风速与边界层位温显著正相关;200 m以下风速与边界层比湿显著负相关;风速对位温和比湿的影响程度均随高度上升而增加。粗糙度对湿地边界层位温的影响高度为60 m,对比湿的影响高度为10~20 m;在影响高度之下粗糙度与位温和比湿均显著正相关,且其影响程度均随高度增加减小;(3)高层大气的位温和比湿变化主要受风速的影响,而低层大气的位温和比湿变化则受到风速和粗糙度的共同影响。

     

    Abstract: To study the vertical structure of temperature and humidity in the atmosphere boundary layer over the homogeneous wetland underlying surface, the twodimensional numerical model was applied to simulate the potential temperature and specific humidity profiles within 1000 m in Honghe National Nature Reserve in the summer of 2008. Besides, the numerical simulation was also used to analyse the correlation between the structure of the atmospheric boundary layer and the two main influence factors (wind velocity and roughness length), and to investigate their effects on the potential temperature and specific humidity at different heights. The results indicated that: (1) The twodimensional numerical model could provide a fair description of the vertical structure of the atmosphere boundary layer over the wetland underlying surface, the simulated results of potential temperature were superior to the results of specific humidity. (2) Wind velocity and roughness length are the main factors influencing temperature and humidity profiles over the wetland underlying surface. Wind velocity performed remarkable positive correlation with potential temperature and negative correlation with specific humidity. Wind velocity had a similar correlation coefficient with potential temperature below 60 m, and significant negative correlation with specific humidity below 200 m. The effect of wind on potential temperature and specific humidity increased with height over wetland. The effective height of roughness length on potential temperature was 60 m, and that on specific humidity was between 10 m and 20 m. Roughness length of wetland underlying surface has a significant positive correlation with potential temperature and specific humidity under the affect altitude, and its influence decreased with inerease in altitude. (3) The variation of potential temperature and specific humidity in high altitude were controlled by wind velocity mainly, but they were both influenced by wind velocity and roughness length in low altitude.

     

/

返回文章
返回