中国农业气象 ›› 2026, Vol. 47 ›› Issue (9): 1485-1495.doi: 10.3969/j.issn.1000-6362.2026.09.010

• 农业生物气象栏目 • 上一篇    下一篇

1961−2024年气候变化对河西走廊酿酒葡萄气候品质的影响

王丽岩,刘峰贵,张硕,任玉玉,陈莉,刘君言   

  1. 1.青海师范大学地理科学学院,西宁 810004;2.北京风云气象科技发展有限公司,北京 100081;3.国家气候中心,北京 100081;4.黑龙江省气候中心,哈尔滨 150030;5.中国社会科学院可持续发展研究中心,北京 100028
  • 收稿日期:2025-06-26 出版日期:2026-09-20 发布日期:2026-09-18
  • 作者简介:王丽岩,E-mail:6066980@qq.com
  • 基金资助:
    国家重点研发计划项目(2019YFA0606902)

Climate Change Impact on the Climate Quality of Wine Grapes in the Hexi Corridor from 1961 to 2024

WANG Li-yan, LIU Feng-gui, ZHANG Shuo, REN Yu-yu, CHEN Li, LIU Jun-yan   

  1. 1. School of Geosciences, Qinghai Normal University, Xi’ning 810004, China; 2. Beijing Fengyun Meteorological Technology Development Co., Ltd., Beijing 100081; 3. National Climate Center, Beijing 100081; 4. Heilongjiang Provincial Climate Center, Harbin 150030; 5. Research Center for Sustainable Development, Chinese Academy of Social Sciences, Beijing 100028
  • Received:2025-06-26 Online:2026-09-20 Published:2026-09-18

摘要:

基于1961−2024年河西走廊17个国家级气象站长序列均一数据,利用趋势分析、突变检验和变化差异检验,分析1961−2024年酿酒葡萄潜在生育期内≥10℃有效积温、水热值、日照时数及采收前降水量与平均气温等关键因子的时空变化特征,评估其对酿酒葡萄气候品质的影响,为河西走廊酿酒葡萄种植适应气候变化提供科学依据。结果表明:1961−2024年河西走廊热量资源显著改善,酿酒葡萄潜在生育期内≥10℃有效积温呈极显著上升趋势(6.1℃·d·a−1,P<0.01),于1997年前后发生突变,潜在生育期内平均有效积温由1169℃·d升至1408℃·d,酿酒葡萄气候品质由一般等级提升至优良等级。1961−2024年河西走廊酿酒葡萄潜在生育期内水热值亦呈极显著上升趋势(11.6℃·mm·a−1,P<0.01),多次突破酿酒葡萄潜在生育期水热值适宜阈值,对张掖、金昌和武威等地酿酒葡萄气候品质产生不利影响。光照资源丰富且持续优化(2.7h·a−1,P<0.01),特别是低海拔地区增温增光趋势明显,对酿酒葡萄气候品质形成具有积极意义。1961−2024年河西走廊酿酒葡萄气候品质总体提升,祁连山东侧的酒泉−高台−武威一带显著上升,种植适宜区向东扩展,但西南山区略有下降。气候变化对酿酒葡萄气候品质的影响具有明显的阈值效应和区域分异特征。河西走廊热量资源和光照资源的增加是酿酒葡萄气候品质提升的主导因素,但过度增温及水热值上升也会引发酿酒葡萄气候品质下降的风险。

关键词: 河西走廊, 气候变化, 酿酒葡萄, 气候品质, 气候风险

Abstract:

Based on the long−term homogeneous data of 17 national meteorological stations in the Hexi corridor from 1961 to 2024, this study analyzed spatiotemporal variation characteristics of effective accumulated temperature of ≥10℃, water heating value, sunshine hours and cumulative precipitation and temperature before harvest during the potential growing period of wine grapes using trend analysis, mutation test and change difference test. The impact of key meteorological factors on the climate quality of wine grapes was assessed to provide a scientific basis for adapting wine grape cultivation to climate change in the Hexi corridor. The results showed that thermal resources had significantly improved, effective accumulated temperature of ≥10℃ showed a significant upward trend (6.1℃·d·y−1, P<0.01) from 1961 to 2024. There was a mutation around 1997, the average effective accumulated temperature during the potential growing period increased from 1169℃·d to 1408℃·d, and improved the climate quality of wine grapes from average to excellent level. Water heat value also showed a significant upward trend (11.6℃·mm·y−1, P<0.01), and multiple thresholds were broken during the potential growth period of wine grapes, leading to adverse effects on the climate quality of wine grapes in Zhangye, Jinchang, Wuwei and other areas. Sunshine resources had become abundant and continuously optimized (2.7h·y−1, P<0.01). The trend of increasing temperature and sunlight was particularly evident in low−altitude areas, which had a positive significance for the quality formation of wine grapes. The overall climate quality of wine grapes had improved in the Hexi corridor, with significant increases in the Jiuquan, Gaotai and Wuwei areas on the eastern side of the Qilian mountains. The area of suitable planting had expanded to the east, while there had been a slight decrease in the southwestern mountainous areas. The study had shown that climate change had a significant threshold effect and characteristics of regional differentiation on the climate quality of wine grapes. The increase in heat and light resources in the Hexi corridor were the dominant factors in improving the climate quality of wine grapes. However, excessive warming and an increase in water heat can also increase the risk of a decline in the climate quality of wine grapes.

Key words: Hexi corridor, Wine grapes, Climate change, Climate quality, Climate risk