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海南岛地区大气输送和扩散特征的数值模拟
引用本文:张振州,蔡旭晖,康凌,吴彬贵.海南岛地区大气输送和扩散特征的数值模拟[J].环境科学学报,2014,34(2):281-289.
作者姓名:张振州  蔡旭晖  康凌  吴彬贵
作者单位:1. 北京大学环境科学与工程学院, 环境模拟与污染控制国家重点联合实验室, 北京 100871;2. 中国人民解放军海军91715部队, 广州 510450;1. 北京大学环境科学与工程学院, 环境模拟与污染控制国家重点联合实验室, 北京 100871;1. 北京大学环境科学与工程学院, 环境模拟与污染控制国家重点联合实验室, 北京 100871;3. 天津市气象科学研究所, 天津 300074
基金项目:国家重点基础研究发展计划项目(No. 2010CB428501);国家自然科学基金项目(No. 41121004,41075004)
摘    要:采用中尺度气象模式WRF及风场诊断模式CALMET,结合轨迹分析和拉格朗日随机游走模拟方法,分析了海南岛地区低层大气中尺度水平输送和扩散特性,并计算了各季平均大气扩散模态.结果表明,该区域大气污染物的扩散和输送主要受到大尺度背景环流、海陆风等局地环流及地形绕流等的影响.海陆风局地环流是沿海城市源排放的大气污染物向海南本岛输送和扩散的主要机制.北部城市海口的大气扩散对岛内影响最大,冬季平均影响范围可覆盖西北半部;春、秋季主要影响西北和北部区域;夏季对本岛的影响仅限于北部沿岸.南部城市三亚的大气扩散对岛内影响较小,秋季向西南海面的扩散对本岛几乎没有影响;冬、春季对三亚以西沿岸的影响有所增加;夏季扩散影响全面指向岛内,并因地形的作用而东、西向大角度扩展,影响海岛南部的大部分沿岸地区.西北部昌江的平均输送扩散方向与当地海岸线的走向基本一致,污染影响不易深入到岛内.其中,秋季扩散影响以偏西南方向为主,仅对昌江西南部分海岸有少量影响;冬、春季扩散形态类似但影响范围扩大到以东方市为代表的低山盆地地带;海岛西北部大部分沿海地带可受到昌江夏季扩散的影响,但平均扩散方向指向东北偏北的海面.

关 键 词:海南岛  大气扩散  WRF  随机游走  轨迹
收稿时间:5/2/2013 12:00:00 AM
修稿时间:2013/5/28 0:00:00

Numerical simulation of atmospheric transport and diffusion over Hainan Island
ZHANG Zhenzhou,CAI Xuhui,KANG Ling and WU Bingui.Numerical simulation of atmospheric transport and diffusion over Hainan Island[J].Acta Scientiae Circumstantiae,2014,34(2):281-289.
Authors:ZHANG Zhenzhou  CAI Xuhui  KANG Ling and WU Bingui
Institution:1. College of Environmental Sciences and Engineering, Peking University, State Joint Key Lab of Environmental Simulation and Pollution Control, Beijing 100871;2. Unit 91715 of PLA Navy, Guangzhou 510450;1. College of Environmental Sciences and Engineering, Peking University, State Joint Key Lab of Environmental Simulation and Pollution Control, Beijing 100871;1. College of Environmental Sciences and Engineering, Peking University, State Joint Key Lab of Environmental Simulation and Pollution Control, Beijing 100871;3. Institute of Meteorology of Tianjin, Tianjin 300074
Abstract:The trajectory analysis and random walk simulation, driven by the meteorological field from WRF and CALMET models, were used to reveal the effects of atmospheric meso-scale transport and diffusion over Hainan Island. Results show that atmospheric transport and diffusion are affected by synoptic winds, local sea-land breezes circulation and orographic effects. The sea breeze circulation is the main mechanism of transporting and spreading air pollutants from coastal source emissions inland. The pollutants from Haikou exert the greatest influence on the main island, with the average sphere of influence covering the northwest half the island in winter, the northwest and northern parts in spring and autumn, and limited to the northern coast in summer. By contrast, the diffusion from Sanya affects the island lightly. The diffusion to the southwest sea causes little effect on air quality over the island. But there is an increase in the influence on the west coast of Sanya in winter and spring. The atmospheric diffusion in summer exercises an overall influence on the southern coastal inland region, which shows a wide-angle expansion along the coast from west to east because of topography. The average transport and diffusion presents a consistent trend with the local coastline. Consequently, it is not easy and smooth for air pollutants to penetrate inland. The diffusion process tends to the southwest in autumn with little effect on southwest seashore of Changjiang. Diffusion behavior in winter and spring presents similar patterns and expands to hilly and basin zone near Dongfang. Most of coastal regions in northwest of the island is under the influence of summer pollutants spreading of Changjiang mainly towards north-northeast sea.
Keywords:Hainan Island  atmospheric diffusion  WRF model  random walk  trajectory analysis
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