Identification of the Non-stationarity of Extreme Temperature Events and Teleconnections with Solar Activity and Large-Scale Atmospheric Circulation: A Case Study in the Yangtze River Economic Belt

Lin Zhang , Jingyun Ling , Shengzhi Huang , Hongbin Zhan , Yi Wu , Menggui Jin , Qiang Huang

Journal of Earth Science ›› : 1 -21.

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Journal of Earth Science ›› :1 -21. DOI: 10.1007/s12583-024-0074-4
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Identification of the Non-stationarity of Extreme Temperature Events and Teleconnections with Solar Activity and Large-Scale Atmospheric Circulation: A Case Study in the Yangtze River Economic Belt
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Abstract

In recent decades, extreme climate events have become a major problem worldwide. To understand the uncertainty in the response of extreme events to global warming, regional assessments are required for various climatic and geographic regions. The spatiotemporal distribution of extreme temperature events in the Yangtze River Economic Belt (YREB) from 1960 to 2019, including interannual changes and their teleconnections with solar activity and large-scale atmospheric circulation, were analyzed using eight indices of extreme temperature events. Over the past six decades, the climate in the YREB region has seen a warming trend, characterized by an increase in extreme warm events and a decrease in extreme cold events. The extreme temperature indices exhibit strong spatial variability. The warm extremes display a significant upward trend across the YREB, while cold extremes are primarily concentrated in the western part of the region. In recent decades, both warm and cold extremes have significant interannual variations, and these events predominantly oscillate over periods of less than four years. After 1985, the relationship between El Niño-Southern Oscillation (ENSO), Arctic Oscillation (AO), and Pacific Decadal Oscillation (PDO) and extreme temperature events has changed significantly compared with pre-1985, and the direction of the phase angle can determine the positive and negative effects of the two time series. The ENSO, AO, and PDO mainly have positive impacts on extreme temperature events, with ENSO and AO exerting greater impacts than PDO. In contrast, solar activity mainly has a negative impact on these events. Furthermore, the notable interdecadal changes in extreme temperature events, especially warm extremes, may be caused by the shift in the PDO phase. Therefore, the results of the study are important for the YREB region to take effective measures to mitigate the potential impacts of human activities on regional warming.

Keywords

extreme temperature events / Yangtze River Economic Belt / climate changes / solar activity / large-scale atmospheric circulation / environmental geology

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Lin Zhang, Jingyun Ling, Shengzhi Huang, Hongbin Zhan, Yi Wu, Menggui Jin, Qiang Huang. Identification of the Non-stationarity of Extreme Temperature Events and Teleconnections with Solar Activity and Large-Scale Atmospheric Circulation: A Case Study in the Yangtze River Economic Belt. Journal of Earth Science 1-21 DOI:10.1007/s12583-024-0074-4

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