Possible influences of spring Barents Sea ice shrinking on Chinese heat wave events

Author:

Qianrong Ma12ORCID,Zhikuan Wang1,Taichen Feng3,Ping Gao4,Yuanyuan Ma5,Pengcheng Yan6,Guolin Feng17ORCID

Affiliation:

1. College of Physical Science and Technology Yangzhou University Yangzhou China

2. Key Laboratory of Meteorological Disaster (KLME), Ministry of Education & Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD) Nanjing University of Information Science & Technology Nanjing China

3. School of Atmospheric Sciences, and Key Laboratory of Tropical Atmosphere‐Ocean System, Ministry of Education Sun Yat‐sen University Zhuhai China

4. Jiangsu Yangzhou Meteorological Bureau Yangzhou China

5. Key Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Northwest Institute of Eco‐Environment and Resources Chinese Academy of Sciences Lanzhou China

6. Key Laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province, Key Laboratory of Arid Climatic Change and Reducing Disaster of China Meteorological Administration Institute of Arid Meteorology of China Meteorological Administration Lanzhou China

7. China Meteorological Administration Key Laboratory for Climate Prediction Studies National Climate Center Beijing China

Abstract

AbstractHeat waves have a catastrophic impact on ecosystems, economy, society and human health. Revealing the underlying physical drivers of heat waves is essential for improving extreme event forecasts and disaster prevention capabilities under climate change. Thus, this study provides an analysis of the maximum temperature, and heat wave frequency and duration during July–August in China from 1961 to 2022. Significant upward trends of different heat wave indexes were observed and broke the historical record in 2022. The influence of large‐scale circulation on heat waves illustrates that the eastward South Asia High (SAH) and anomalously westward Western Pacific Subtropical High (WPSH) are closely associated with increased heat wave events, especially in 2022. We further demonstrate using reanalysis data that the Barents Sea ice shrinkage is associated with increased heat waves in China by modulating favourable atmospheric circulations. In addition, the North Atlantic Oscillation (NAO), which is closely linked to Arctic Sea ice, can provoke large‐scale Rossby waves, which in turn can cause extreme heat events in China. In particular, the reduced sea ice coupled with NAO strengthens the anomalous eastward SAH and anomalous westward WPSH of their position and intensity especially in 2022 and provides favourable atmospheric circulation patterns for the occurrence of heat waves.

Funder

National Natural Science Foundation of China

Key Laboratory of Meteorological Disaster, Ministry of Education

Natural Science Foundation of Tibet Autonomous Region

Publisher

Wiley

Subject

Atmospheric Science

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