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干旱区地理 ›› 2025, Vol. 48 ›› Issue (7): 1141-1152.doi: 10.12118/j.issn.1000-6060.2024.437 cstr: 32274.14.ALG2024437

• 气候与水文 • 上一篇    下一篇

气候变化及新四季划分方法下的西藏季节变化趋势分析

史继清1,2(), 罗珍1, 益西卓玛1, 刘赛3(), 李积宏4, 旦增益嘎1, 甘臣龙5   

  1. 1.西藏自治区气候中心,西藏 拉萨 850000
    2.日喀则国家气候观象台,西藏 日喀则 857000
    3.西藏自治区气象灾害防御技术中心,西藏 拉萨 850000
    4.那曲市气象局,西藏 那曲 852000
    5.墨竹工卡县气象局,西藏 拉萨 850000
  • 收稿日期:2024-07-19 修回日期:2024-09-05 出版日期:2025-07-25 发布日期:2025-07-04
  • 通讯作者: 刘赛(1992-),男,本科,工程师,主要从事生态方面的研究. E-mail: liusaiotl@163.com
  • 作者简介:史继清(1988-),女,硕士研究生,副研级高工,主要从事农业气象灾害方面的研究. E-mail: shijiqing10@126.com
  • 基金资助:
    中国气象局公共气象服务中心创新基金项目(M2021015);区域创新发展联合基金重点支持项目(U23A2006);西藏自治区科技创新基地建设项目(XZ202401YD0008);西藏自治区科技计划重点研发及转化项目(XZ202401ZY0065)

Trend analysis of seasonal changes in Xizang based on climate change and new seasonal division

SHI Jiqing1,2(), LUO Zhen1, YIXI Zhuoma1, LIU Sai3(), LI Jihong4, DANZENG Yiga1, GAN Chenlong5   

  1. 1. Xizang Climate Center, Lhasa 850000, Xizang, China
    2. Xigazê National Climate Oberservatory, Xigazê 857000, Xizang, China
    3. Xizang Meteorological Disaster Prevention Technology Center, Lhasa 850000, Xizang, China
    4. Nagqu Meteorological Bureau, Nagqu 852000, Xizang, China
    5. Maizhokunggar County Meteological Bureau, Lhasa 850000, Xizang, China
  • Received:2024-07-19 Revised:2024-09-05 Published:2025-07-25 Online:2025-07-04

摘要: 基于1981—2023年西藏38个气象站点气温日资料,选择西藏新四季划分方法划分西藏四季,探讨西藏气候季节区域变化、四季开始日期的时空变化以及季节变化趋势。结果表明:(1) 西藏四季分明区集中分布在雅鲁藏布江一线和林芝市,四季不分明区(无夏区)主要位于西藏西部、北部和沿喜马拉雅山一带的高海拔区域。(2) 西藏春、夏季开始日期有提前的趋势,秋、冬季开始日期有推迟的趋势。春季开始日期于2000年出现显著提前突变,秋、冬季开始日期分别于2003、1995年出现显著推迟突变。(3) 就开始日期而言,春、秋季的第一模态(EOF1)呈现“春季西北低、东南高,秋季中间高、两边低”的特点;春季的第二模态(EOF2)表现为“西北正、东南负”的反向分布型;秋季EOF2呈现西南正值中心与东北负值中心相反的空间分布特征;冬季EOF1属于“北部高、西南部低”,冬季EOF2与春季EOF2特征相同。(4) 未来春、夏季开始日期的推迟和秋、冬季提前的态势将出现。

关键词: 开始日期, 小波分析, 趋势分析, 经验正交函数(EOF), 西藏

Abstract:

This study analyzes daily temperature data from 38 meteorological stations in Xizang, China, covering the period from 1981 to 2023. A new method for seasonal division in Xizang was employed to categorize the four seasons, and the regional climate changes, temporal shifts in the start dates of each season, and trends in seasonal changes were examined. The results show the following. (1) Areas with four distinct seasons in Xizang are primarily found along the Yarlung Zangbo River and in Nyingchi City, whereas regions with less distinct seasonal variations (including areas without a summer season) are mainly situated in the western and northern parts of Xizang as well as in the high-altitude regions of the Himalayas. (2) In Xizang, the beginning of spring and summer tends to occur earlier, whereas the onset of autumn and winter tends to be delayed. Notably, the start date of spring was significantly earlier in 2000, whereas the onset of autumn and winter was significantly delayed in 2003 and 1995, respectively. (3) Regarding the timing of seasonal starts, the first empirical orthogonal function (EOF1) for spring and autumn exhibited a pattern of “northwest low and southeast high in spring, and middle high and both sides low in autumn”. In spring, the second EOF (EOF2) presented a contrasting distribution pattern of “northwest positive and southeast negative”, whereas in autumn, EOF2 showed an opposite spatial distribution pattern characterized by “southwest positive and northeast negative”. The EOF1 in winter revealed a “high in the north and low in the southwest” pattern, whereas the EOF2 shared similarities with that of spring’s EOF2. (4) Looking ahead, we anticipate that the start dates of spring and summer will be delayed, whereas those for autumn and winter will be advanced.

Key words: start date, wavelet analysis, trend analysis, empirical orthogonal function (EOF), Xizang