Y. Dian-Xiu Author informationContact: ydx@cma.gov.cnNational Climate Center, China Meteorological Administration, Beijing 100081, China , Y. Ji-Fu Author informationSchool of Atmospheric Physics, Nanjing University of Information Science & Technology, Nanjing 210044, ChinaKey Laboratory for Aerosol-Cloud-Precipitation of China Meteorological Administration, Nanjing University of Information Science and Technology, Nanjing 210044, China , C. Zheng-Hong Author informationHubei Meteorological Service Center, Wuhan 430074, ChinaHubei Service Center for Meteorological Science & Technology, Hebei Meteorological Bureau, Wuhan 430074, China , Z. You-Fei Author informationSchool of Environment Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, ChinaJiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Nanjing University of Information Science & Technology, Nanjing 210044, China , W. Rong-Jun Author informationJiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control, Nanjing University of Information Science & Technology, Nanjing 210044, China
Daily maximum temperatures from 753 stations across China and the heat wave indicators are used to study the temporal and spatial characteristics of heat wave intensity, frequency and heat wave days in China over the period of 1961–2010. The results show that high frequency, long duration and strong intensity of heat waves occurred in the Jianghuai area, Jiangnan area, and eastern Sichuan Basin. The highest frequency and the longest duration are located in northern Jiangxi and northern Zhejiang provinces, and the highest intensity in northern Zhejiang province is even more prominent. The frequency, heat wave days and intensity showed a general increasing trend in the past 50 years, while decadal characteristics are also observed with a decreasing trend from the 1960s to the early 1980s and increasing trend from the end of the 1980s to 2010. The regional variations demonstrate a significant increasing trend in the northern and western parts of North China, central-northern part of Northwest China, the central part of South China, the Yangtze River Delta and the southern Sichuan Basin, with an obvious decreasing trend in the southern Huanghuai area, northern Jianghuai area and Hanjiang River Basin. Ye, D.-X., Yin, J.-F., Chen, Z.-H., et al., 2014. Spatial and temporal variations of heat waves in China from 1961 to 2010. Adv. Clim. Change Res. 5(2), doi: 10.3724/SP.J.1248.2014.066.
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Published on 15/05/17Submitted on 15/05/17
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