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作 者:陈春丽 叶栋水 邱新法[1] 叶秀枝 张玉琴 朱晓晨 CHEN Chunli;YE Dongshui;QIU Xinfa;YE Xiuzhi;ZHANG Yuqin;ZHU Xiaochen(School of Applied Meteorology,Nanjing University of Information Science&Technology,Nanjing 210044,China;Quanzhou Meteorological Bureau,Fujian Quanzhou 362000,China;Fujian Meteorological Information Center,Fuzhou 350000,China;Jinjiang Meteorological Bureau,Fujian Jinjiang 362200,China;Fujian Institute Meteorological Sciences of Province,Fuzhou 350000,China)
机构地区:[1]南京信息工程大学应用气象学院,南京210044 [2]泉州市气象局,福建泉州362000 [3]福建省气象信息中心,福州350000 [4]晋江市气象局,福建晋江362200 [5]福建省气象科学研究所,福州350000
出 处:《气象科学》2020年第2期257-263,共7页Journal of the Meteorological Sciences
基 金:国家自然科学青年科学基金资助项目(41805049)。
摘 要:利用2017年晋江市及其周边共27个自动气象站逐小时气象资料,分析了2017年晋江城市热岛强度的日变化及有无海陆风对城市热岛强度的影响,同时研究了不同季节海陆风风速对城市热岛强度的影响,最后通过典型个例海陆风日验证了晋江城市热岛的日变化特征。结果表明:晋江市全年平均热岛强度的日变化趋势呈“V”字型分布;海风能使城市降温,减弱城市热岛强度,而陆风能使夜间热岛显著增强,故与非海陆风日相比,海陆风日热岛强度的日变化幅度增大;热岛强度与海陆风风速呈负相关,海陆风风速越大对城市热岛有一定的缓解作用。Based on the hourly meteorological data from 27 automatic meteorological stations in Jinjiang and its surrounding areas in 2017,the diurnal variation of urban heat island intensity in Jinjiang in 2017 and the influence of sea-land breeze on urban heat island intensity were analyzed.Moreover,the influence of sea-land breeze speed in different seasons on the urban heat island intensity was also studied.Finally,the diurnal variation characteristics of urban heat island in Jinjiang were verified by a typical day with sea-land breeze.The results show that the annual average heat island intensity in Jinjiang City has a V-shaped diurnal variation trend;the sea breeze cools the city,and weakens the urban heat island intensity,while the land breeze can significantly enhance the heat island at night.Thus,the durinal variation of the heat island intensity at the day with sea-land breeze increases,compared with the day without sea-land breeze.The heat island intensity is negatively correlated with the sea-land breeze speed.The faster sea-land breeze speed can alleviate the urban heat island to some extent.
分 类 号:P463.3[天文地球—大气科学及气象学]
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