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Arid Land Geography ›› 2026, Vol. 49 ›› Issue (5): 907-916.doi: 10.12118/j.issn.1000-6060.2025.423

• Climate Change • Previous Articles     Next Articles

Climate response and operational impact of updated climatological normals in Xizang

CI Wang1(), DU Jun1, ZHAXI Dunzhu2, CHEN Xianyan3(), XIAO Zhuojing1, PINGCUO Sangdan4, LIU Sai5   

  1. 1 Xizang Climate Centre, Lhasa 850000, Xizang, China
    2 Xizang Meteorological Weather Modification Center, Lhasa 850000, Xizang, China
    3 National Climate Center, China Meteorological Administration, Beijing 100081, China
    4 Xizang Institute of Plateau Atmospheric and Environmental Science Research, Lhasa 850000, Xizang, China
    5 Xizang Meteorological Disaster Prevention Technology Center, Lhasa 850000, Xizang, China
  • Received:2025-07-17 Revised:2025-08-19 Online:2026-05-25 Published:2026-05-25
  • Contact: CHEN Xianyan E-mail:Tcc_ciwang@126.com;chenxy@cma.gov.cn

Abstract:

To understand the impact of updating climatological normals on climate characteristics and operational assessments in Xizang of China, Based on the data of 38 national meteorological stations in Xizang from 1981 to 2023, the effects of updating the old and new climatological normals values from 1981 to 2010 and from 1991 to 2020 on climate change and business were analyzed. The results reveal the following: (1) Under the new climatological normals, the climate in Xizang is warmer and wetter than under the previous normals, with the annual mean temperature increasing by 0.3 ℃ and annual precipitation increasing by 2.0%. Annual mean temperature increases are more pronounced in the western, northern, and northeastern regions, while annual mean precipitation shows uneven spatial distribution. (2) Updating climatological normals significantly affects climate-related operations, such as the identification of warm winter events and the probability of extreme high and low temperatures. Under the new normals, the number of regional warm winter years in Xizang over the past 43 years decreased from 18 years to 9 years. (3) Based on the new climatological normals, the number of (significantly) high annual mean temperature years decreased from 16 years to 9 years, whereas the number of (significantly) low annual mean temperature years increased from 6 years to 12 years, resulting in a shift in the average temperature evaluation from high to low categories. The frequency of extreme high-temperature seasons decreases, whereas low-temperature years (seasons) increase. (4) The frequency of above-normal spring and summer years decreases, whereas above-normal autumn years increase. Meanwhile, the likelihood of extreme heavy precipitation increases in autumn but decreases in spring and summer. The observed changes, such as the reduction in warm winter years and the apparent increase in the probability of extreme low-temperature events, are primarily attributable to elevated statistical thresholds associated with warmer climatological normals. This reflects a statistical reconstruction effect rather than an actual cooling trend or a real increase in extreme cold events in Xizang.

Key words: updated climatological normals, climate assessment system, extreme climate events, Xizang