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Sudden stratospheric warming linked to extreme cold weather in North India: Physical processes and impacts

气候学 环境科学 平流层突然变暖 极寒 极端天气 气象学 大气科学 气候变化 地理 平流层 极涡 地质学 海洋学
作者
K S Athira,Raju Attada,Mathew Barlow,V. Brahmananda Rao
出处
期刊:Quarterly Journal of the Royal Meteorological Society [Wiley]
卷期号:152 (774) 被引量:1
标识
DOI:10.1002/qj.70020
摘要

Abstract The 2024 winter season was peculiar, with North India experiencing an intense and prolonged cold wave (CW) in January 2024, lasting for six consecutive days (spanning from the 21st to the 26th) in the absence of a usual western disturbance propagation. Our findings indicate that this CW was a result of the sudden stratospheric warming (SSW) that occurred on 16th and 17th January 2024. The SSW caused the polar vortex to shift towards lower latitudes (southward), advecting cold Arctic air to the lower latitudes of North Asia and Europe. This cold air mass then gradually moved eastward, eventually settling over East Asia. Consequently, a ‘ dipole block ’ developed and strengthened, as a result of the SSW, over the Siberian‐East Asian region, with the ridge centered over Siberia. The downstream portion of this ridge transported cold air from East Asia to North India, leading to the CW. The blocking pattern also keeps weather systems stagnant for longer periods, contributing to the prolonged CW conditions. Thus, the SSW event indirectly led to the CW in North India. We further examined the impact of SSW on CWs and found that, in addition to the CW in 2024, the CW events in the winters of 2004 and 2019 were also associated with SSWs. A common characteristic feature associated with all three SSW‐related CWs is the formation of an atmospheric block that is strengthened by the downward propagation of the stratospheric signal to the troposphere. Lastly, we made use of the two biometeorological indicators – the Universal Thermal Climate Index and the Wind Chill Index (WCI) – to study the implications of the 2024 CW event. It is observed that slight cold stress first emerges over the Indo‐Gangetic Plains, which later expands to the northern parts of the country, particularly between 18:00 and 23:00 Indian Standard Time (IST). A moderate cold stress is experienced in isolated pockets of North and Northwest India between 0:00 and 7:00 IST. WCI indicates discomfort predominating during the evening, night, and early morning hours due to higher wind speeds along with the low temperatures.
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