The Influence of El Niño Events on the Climate of Northeastern China: An Integrated Analysis
DOI:
https://doi.org/10.61173/4mbe9231Keywords:
El Niño, Global Warming, China Climate, Extreme Weather, 2023 Temperature RecordsAbstract
The year 2023 has been projected to be potentially the warmest year since 1850, largely attributed to the El Niño phenomenon, highlighting its significant impact on global climate patterns, including those affecting China [1] The occurrence of El Niño has been linked to extreme weather transitions in China, from unusually warm conditions to sudden freezing temperatures, underscoring the variability and extremity introduced by this climatic event [2]. Research further suggests that the combination of El Niño and the Atlantic Multidecadal Oscillation (AMO) has contributed to the remarkably large margin of global temperature increases observed in 2023 [3]. This assertion is supported by the World Meteorological Organization’s confirmation that 2023 has indeed shattered global temperature records, emphasizing the profound influence of El Niño on exacerbating climate anomalies worldwide, including in China[4]. This study aims to delve deeper into the mechanisms through which El Niño influences China’s climate, particularly focusing on temperature variations and the incidence of extreme weather events, to understand better the broader implications of such climatic phenomena on regional and global scales.
References
[1] China Daily Global. (2023). 2023 could be warmest year since 1850 due to El Nino. Retrieved from http:// global.chinadaily.com.cn
[2] Reuters. (2023). China set for sudden change from warm to freezing in year of extreme. Retrieved from http://www.reuters.com
[3] Springer. (2023). El Niño and the AMO Sparked the Astonishingly Large Margin. Retrieved from http://link. springer.com
[4] World Meteorological Organization. (2023). WMO confirms that 2023 smashes global temperature record. Retrieved from http://wmo.int
[5] Sarachik ES, Cane MA. The El Niño-Southern Oscillation phenomenon. London: Cambridge University Press;
[6] Yeh SW, Cai W, Min SK, McPhaden MJ, Dommenget D, Dewitte B, Collins M, Ashok K, An SI, Yim BY, et al. ENSO atmospheric teleconnections and their response to greenhouse gas forcing. Rev Geophys. 2018;56:185–206.
[7] Zuo H, Balmaseda MA, Tietsche S, Mogensen K, Mayer M. The ECMWF operational ensemble reanalysis– analysis system for ocean and sea ice: A description of the system and assessment. Ocean Sci. 2019;15:779–808.
[8] Meinen CS, McPhaden MJ. Observations of warm water volume changes in the equatorial Pacific and their relationship to El Niño and La Niña. J Clim. 2000;13:3551– 3559.
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