Journal
ADVANCES IN CLIMATE CHANGE RESEARCH
Volume 12, Issue 6, Pages 795-803Publisher
SCIENCE PRESS
DOI: 10.1016/j.accre.2021.10.005
Keywords
Precipitation events; Northwest China; CMIP5; Fraction of attributable risk; Attribution analysis
Funding
- Project of Tianshan Innovation Team in Xinjiang [202113050]
- Chinese Academy of Sciences President's International Fellowship Initiative [2017VCA0002]
- Met Office Hadley Centre Climate Programme - Department for Business, Energy and Industrial Strategy and Department for Environment, Food and Rural Affairs
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Extreme rainfall events in inland arid regions have been occurring more frequently in recent years and causing significant casualties and economic losses. The heavy rains in Hami prefecture of eastern Xinjiang, China in 2018 were mainly caused by an abnormal weather system transporting abundant water vapor from the Indian Ocean and East China Sea, leading to devastating floods. The study suggests a significant human influence on the risk of extreme rainfall events, highlighting the importance of better managing water-related disasters in arid regions.
Extreme rainfall events are rare in inland arid regions, but have exhibited an increasing trend in recent years, causing many casualties and substantial socioeconomic losses. A series of heavy rains that began on July 31st, 2018, battered the Hami prefecture of eastern Xinjiang, China for four days. These rains sparked devastating floods, caused 20 deaths, eight missing, and the evacuation of about 5500 people. This study examines the extreme rainfall event in a historical context and explores the anthropogenic causes based on analysis of multiple datasets (i.e., the observed daily data, the global climate models (GCMs) from the Coupled Model Intercomparison Project Phase 5 (CMIP5), the NCEP/NCAR Reanalysis 1, and the satellite cloud data) and several statistical techniques. Results show that this extraordinarily heavy rainfall was due mainly to the abnormal weather system (e.g., the abnormal subtropical high) that transported abundant water vapor from the Indian Ocean and the East China Sea crossed the high mountains and formed extreme rainfall in Hami prefecture, causing the reservoir to break and form a flood event with treat loss, which is a typical example of a comprehensive analysis of the extreme rainfall event in summer in Northwest China. Also, the fraction of attributable risk (FAR) value was 1.00 when the 2018 July-August RX1day (11.52 mm) was marked as the threshold, supporting the claim of a significant anthropogenic influence on the risk of this extreme rainfall. The results offer insights into the variability of precipitation extremes in arid areas contributing to better manage water-related disasters.
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