The extreme high temperature anomaly(EHTA) events in a region are one of the most important
climatic parameters to make climate assessment of the trend of regional climate
change. The diagnosis and analysis of the EHTA event in Zhejiang Province in
East China in 2022 show that the event has set the rarest record in this region in the past 71 years from both time and
space perspectives. The results of Mann-Kendall trend analysis showed that the
mean annual high temperature days in Zhejiang Province had a sudden change. The
sudden change occurred around 2004, and the trend was rising after the sudden
change.
References
[1]
Ding, T., Qian, W.H. and Yan, Z.W. (2010) Changes in Hot Days and Heat Waves in China during 1961-2007. International Journal of Climatology, 30, 1452-1462. https://doi.org/10.1002/joc.1989
[2]
Ding, T. and Ke, Z.J. (2015) Characteristics and Changes of Regional Wet and Dry Heat Wave Events in China during 1960-2013. Theoretical and Applied Climatology, 122, 651-665. https://doi.org/10.1007/s00704-014-1322-9
[3]
Du, Y.D., AIH, Duan, H.L., et al. (2013) Changes in Climate Factors and Extreme Climate Events in South China during 1961-2010. Advances in Climate Change Research, 4, 1-11. https://doi.org/10.3724/SP.J.1248.2013.001
[4]
Gong, Z.Q., Wang, Y.J., Wang, Z.Y., et al. (2014) Briefly Analysis on Climate Anomalies and Causations in Summer 2013. Meteorological Monthly, 40, 119-125.
[5]
Hou, W., Chen, Y., Li, Y., et al. (2014) Climate Characteristics over China in 2013. Meteorological Monthly, 40, 482-493.
[6]
Huang, L., Chen, A.F., Zhu, Y.H., et al. (2015) Trends of Temperature Extremes in Summer and Winter during 1971-2013 in China. Atmospheric and Oceanic Science Letters, 8, 220-225. https://doi.org/10.1080/16742834.2015.11447263
[7]
Hu, L.S., Huang, G. and Qu, X. (2017) Spatial and Temporal Features of Summer Extreme Temperature over China during 1960-2013. Theoretical and Applied Climatology, 128, 821-833. https://doi.org/10.1007/s00704-016-1741-x
[8]
Jia, J. and Hu, Z.Y. (2017) Spatial and Temporal Features and Trend of Different Level Heat Waves over China. Advances in Earth Science, 32, 546-559. (In Chinese)
[9]
Lin, P.F., He, Z.B., Du, J., et al. (2017) Recent Changes in Daily Climate Extremes in an Arid Mountain Region, a Case Study in North Western China’s Qilian Mountains. Scientific Reports, 7, 2245. https://doi.org/10.1038/s41598-017-02345-4
[10]
Liu, H.Z., Zhao, S.R., Zhao, C.G., et al. (2006) Weather Abnormal and Evolution of Western Pacific Subtropical High and South Asian High in Summer of 2003. Plateau Meteorology, 25, 169-178.
[11]
Qi, X.H., Chen, Y., Li, D.M., et al. (2016) A Review of Western High Temperature Heat Wave Research. Acta Ecologica Sinca, 36, 2773-2778. https://doi.org/10.5846/stxb201503170507
[12]
Qian, C., Zhang, B. and Li, Z. (2019) Linear Trends in Temperature Extremes in China, with an Emphasis on Non-Gaussian and Serially Dependent Characteristics. Climate Dynamics, 53, 533-550. https://doi.org/10.1007/s00382-018-4600-x