中国农业气象 ›› 2025, Vol. 46 ›› Issue (3): 290-304.doi: 10.3969/j.issn.1000-6362.2025.03.002

• 农业生态环境栏目 • 上一篇    下一篇

新气候态背景下青海高原气候生产潜力评估

孙文慧,索琳,傅永超,李金海,韩琳   

  1. 1.青海省防灾减灾重点实验室,西宁 810001;2.海东市气象局,海东 810600;3.海北州祁连县气象局,海北 810400;4.青海省气象局,西宁 810001;5.成都信息工程大学大气科学学院,成都 610225
  • 收稿日期:2024-03-19 出版日期:2025-03-20 发布日期:2025-03-19
  • 作者简介:孙文慧,E-mail:389274882@qq.com
  • 基金资助:
    科技部第二次青藏高原科学考察−极端天气气候事件与灾害风险项目(2019QZKK104);青海省气象局“揭榜挂帅”项目(QXGS2024−02)

Assessment of Climatic Productive Potential on the Qinghai Plateau in the Context of the New Climate State Background

SUN Wen-hui,SUO Lin,FU Yong-chao,LI Jing-hai,HAN Lin   

  1. 1.Key Laboratory of Disaster Prevention and Mitigation in Qinghai Province,Xining 810001, China; 2.Meteorological Bureau of Haidong, Haidong 810600; 3.Qilian Meteorological Bureau, Haibei 810400; 4.Qinghai Meteorological Bureau, Xining 810001; 5.School of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225
  • Received:2024-03-19 Online:2025-03-20 Published:2025-03-19

摘要:

利用青海高原50个气象站1991−2022年逐日气温和降水数据,基于MiamiThornthwaite Memorial模型,采用数理统计、R/S分析等方法评估新气候态背景下青海高原的气候资源及气候生产潜力。结果表明:1)新气候态下青海高原气候总体趋于暖湿,年平均气温气候倾向率为0.46℃·10a−1(P<0.01),同德增暖明显;年降水量气候倾向率为23.6mm·10a−1(P<0.01),贵南增湿明显。2)新气候态下青海高原气候生产潜力气候倾向率为27.7g·m−2·10a−1(P <0.01),呈显著上升趋势,空间分布差异大。3气候生产潜力的增加与气温升高降水增多有关,气候暖湿化利于气候生产潜力的增加。4青海高原气候生产潜力时空变化特征与降水量变化更接近,降水是气候生产潜力的最主要影响因素。(5)青海高原平均气温、年降水量和气候生产潜力的Hurst指数分别为0.480.280.36,未来趋势与过去相反,气候可能趋于冷干气候生产潜力将下降。

关键词: 青海高原, 气候生产潜力, 新气候态, Thornthwaite Memorial模型, Hurst指数

Abstract:

Based on the temperature and precipitation data from 50 meteorological stations on the Qinghai plateau from 1991 to 2022, the climate resources and climatic productive potential of the Qinghai plateau were evaluated by using the Miami and Thornthwaite Memorial models, mathematical statistics and R/S analysis under the background of the new climatic state. The results showed that: (1)the overall climate of the Qinghai plateau in the new climate state tended to be warm and humid, with an annual average temperature trend rate of 0.46℃·10 y−1(P<0.01), with a significant warming in Tongde. The climate tendency rate of annual precipitation was 23.6mm·10y−1(P<0.01), and there was a significant increase in humidity in Guinan. (2)The climate tendency rate of climatic productive potential on the Qinghai plateau was 27.7g·m−2·10y−1(P<0.01), showing a significant upward trend. In addition, there were significant spatial differences in the climatic productive potential of the Qinghai plateau. (3)The increase in climatic productive potential was related to increase temperatures and precipitation. The climate warming and humidification were conducive to the increase in climatic productive potential. (4)The variation characteristics of the spatiotemporal distribution of climatic productive potential on the Qinghai plateau were closer to the trend of precipitation and precipitation was the most important factor affecting climatic productive potential. (5)The Hurst indices for average temperature, annual precipitation and climatic productive potential on the Qinghai plateau were 0.48, 0.28 and 0.36, respectively. The future trend was opposite to the past, and the climate may tend to be cold and dry, resulting in a continuous decline in climatic productive potential.

Key words: Qinghai plateau, Climatic productive potential, New climate state, Thornthwaite Memorial model, Hurst index