城市地表特征对京津冀地区夏季降水的影响研究  

Impact of Urban Surface Characteristics on Summer Rainfall in the Beijing–Tianjin–Hebei Area

作　　者：张珊[1,2] 黄刚[1,3] 王君[2,4] 刘永[5] 贾根锁[4] 任改莎 

机构地区：[1]中国科学院大气物理研究大气科学和地球流体力学数值模拟国家重点实验室,北京100029 [2]中国科学院大学,北京100049 [3]全球变化研究协同创新中心,北京100875 [4]中国科学院大气物理研究所东亚区域气候-环境重点实验室,北京100029 [5]中国科学院大气物理研究所季风系统研究中心,北京100029 [6]石家庄市鹿泉区气象局,石家庄050200

出　　处：《大气科学》2015年第5期911-925,共15页Chinese Journal of Atmospheric Sciences

基　　金：国家重点基础研究发展计划(973计划)项目2011CB309704;全球变化研究国家重大科学研究计划项目2012CB955604;国家自然科学基金项目41425019;41275083;91337105;高原大气与环境四川省重点实验室开放课题PAEKL-2014-K2

摘　　要：本文利用京津冀地区24个气象站的日降水资料和耦合有单层城市冠层模式（SLUCM）的中尺度数值模式 WRF 的模拟结果，研究了城市地表特征对京津冀地区夏季降水的影响。结果表明，在京津冀城市面积迅速增长的近三十年（1981～2010），该地区大部分站点的降水量都呈现减少的趋势，减少最明显的站点主要集中在京津唐城市区域，其中≥50 mm的降水量减少趋势占总降水量减少趋势的50%以上。城市扩张可能是造成京津冀降水时空格局改变的因素之一。通过对比分析控制试验与敏感性试验的模拟结果，发现城市化引起的地表特征的改变使北京、天津、唐山主要城市地区的降水量和降水频次都有明显减少，而城市群下风向的降水量和降水强度则明显增加和增强，其中50 mm以上等级的降水量变化最为显著，贡献率在60%以上。城市地表特征使北京、天津和唐山地区50 mm以上等级降水量的百分比下降了6%～20%，下风向地区增加了8%。城市地表特征也影响了主要城市和城市群下风向地区降水量的日变化结构，使北京和唐山几乎所有时段的降水量都有所减少，而城市群下风向降水量的增加主要发生在白天。研究发现城市地表特征对深对流的抑制（加强）可能是造成京津冀地区降水减少（增多）的重要原因，而由于城市地表蒸发量的改变引起的潜热通量和对流有效位能的改变则可能是引起深对流变化的重要因素。Utilizing daily precipitation data from 24 meteorological stations and results from the Weather Research and Forecasting （WRF） model / Urban Canopy Model （UCM）, the impact of urban surface characteristics on summer rainfall in the Beijing–Tianjin–Hebei area was investigated. Results indicated that precipitation at most sites in this region has reduced during the last 30 years, and those sites whose precipitation has reduced the most are mainly centered in the Beijing–Tianjin–Tangshan metropolis. Urbanization is one of the possible factors affecting the precipitation in the Beijing–Tianjin–Hebei area. Comparison of the model results from the control run and sensitivity run indicated that rainfall and rainfall frequency clearly decreased in the Beijing–Tianjin–Tangshan metropolis due to the urban surface. Meanwhile, an increase in rainfall and rainfall intensity was apparent downwind of the urban agglomeration; precipitation above 50 mm changed significantly due to the urban surface, and the contribution to the total could be more than 60%. The percentage of rainfall above 50 mm declined by 6%–20% in the Beijing–Tianjin–Tangshan metropolis, while it increased by 8% downwind. The diurnal structure of rainfall changed due to urbanization： precipitation in Beijing and Tangshan mainly reduced due to urbanization, and the increase downwind occurred mainly in daytime. The findings of this study suggest that the inhibition or enhancement of deep convection, as influenced by changes in latent heat flux and convective available potential energy due to the urban surface, may explain the changes in precipitation.

关 键 词：京津冀 城市地表特征 城市化 降水 

分 类 号：P461[天文地球—大气科学及气象学]