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1951—2017年鞍山市气温变化特征及城市热岛变化
引用本文:金巍,刘卫华,李晶,康晓玉. 1951—2017年鞍山市气温变化特征及城市热岛变化[J]. 气象与环境学报, 2021, 37(4): 78-85. DOI: 10.3969/j.issn.1673-503X.2021.04.011
作者姓名:金巍  刘卫华  李晶  康晓玉
作者单位:鞍山市气象局,辽宁 鞍山114000;中国科学院空间天气学国家重点实验室,北京100190;大连气象信息中心,辽宁 大连116001;辽宁省气象信息中心,辽宁 沈阳110166;鞍山市气象局,辽宁 鞍山114000
基金项目:辽宁省气象局关键技术项目(LNG201901);2019年中国科学院国家空间科学中心空间天气学国家重点实验室开放课题(Y92612A55S);辽宁省气象局自筹项目(2019XSG11)
摘    要:
利用建站以来鞍山站和海城乡村站的一日四次观测数据和逐日平均、最低和最高气温资料,对1951—2017年鞍山市年、四季和各月平均气温和极端气温变化特征及其变率进行了分析,并对鞍山城市热岛变化进行探讨.结果表明:1951—2017年鞍山市年平均最低气温的递增趋势最强、平均气温次之、平均最高气温最弱,且均通过显著性检验.19...

关 键 词:气温变化  城市热岛  突变  气候变暖
收稿时间:2020-03-30

Change characteristics of air temperature and urban heat island in Anshan from 1951 to 2017
Wei JIN,Wei-hua LIU,Jing LI,Xiao-yu KANG. Change characteristics of air temperature and urban heat island in Anshan from 1951 to 2017[J]. Journal of Meteorology and Environment, 2021, 37(4): 78-85. DOI: 10.3969/j.issn.1673-503X.2021.04.011
Authors:Wei JIN  Wei-hua LIU  Jing LI  Xiao-yu KANG
Affiliation:1. Anshan Meteorological Service, Anshan, 114000, China2. State Key Laboratory of Space Weather, Chinese Academy of Sciences, Beijing 100190, China3. Dalian Meteorological Information Center, Dalian, 116001, China4. Liaoning Provincial Meteorological Information Center, Shenyang 110166, China
Abstract:
Based on the data of daily mean, minimum and maximum air temperatures observed four times per day in the Anshan region from 1951 to 2017, the change characteristics of the annual, seasonal, and monthly mean air temperatures and extreme air temperatures and their variation ratios as well as the variation of urban heat island were analyzed. The results showed that the increasing trend is strongest for the annual mean minimum air temperature followed by the mean air temperature and is the weakest for the average maximum air temperature in Anshan in the studied period, and all these results have passed the significance test. The annual extreme maximum air temperature in Anshan shows a weak decreasing trend from 1951 to 2017 and experiences a decreasing trend from 1951 to 1987 (before the mutation) and an increasing trend from 1988 to 2017 (after the mutation). Inversely, the annual extreme minimum air temperature shows a significant increasing trend from 1951 to 2017, and a stronger increasing trend from 1951 to 1987 (before the mutation) relative to the former, while shows a decreasing trend from 1988 to 2017 (after the mutation). On the whole, the variations of extreme maximum and minimum air temperatures before and after the mutation are opposite. From 1958 to 2017, urban heat island intensity in Anshan is the largest for annual minimum air temperature, followed by the mean air temperature, and is the smallest for the maximum air temperature with the weakest increasing trend. The intensities of the urban heat island in Anshan in autumn and winter are stronger than in other seasons with a significantly increasing heat island index. Among the four regular temperature observations per day, the intensity of the heat island in Anshan is the smallest at 14 o'clock and the largest at 02 o'clock, and the heat island index shows a decreasing trend at 14 o'clock and a significantly increasing trend at the other times. The mean air temperature in Anshan shows a significantly increasing trend. The intensity of urban heat island and the heat island index in Anshan both increase significantly, especially at nighttime, indicating that the significant increase of the intensity of urban heat islands is one of the main reasons for climate warming in Anshan.
Keywords:Air temperature change  Urban heat island  Mutation  Climate warming  
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