中国农业气象 ›› 2025, Vol. 46 ›› Issue (11): 1529-1545.doi: 10.3969/j.issn.1000-6362.2025.11.001

• 农业气候资源与气候变化栏目 •    下一篇

暖湿化背景下1981−2020年西藏地区大气饱和水汽差时空变化及其成因

杜军,高佳佳,平措桑旦,索朗,扎西旺拉   

  1. 1.西藏高原大气环境科学研究所/西藏高原大气环境开放实验室,拉萨 850001;2.中国气象局墨脱大气水分循环综合观测野外科学试验基地/墨脱国家气候观象台/墨脱大气水分循环西藏自治区野外科学观测研究站,墨脱 860700;3.中国气象局日喀则国家气候观象台,日喀则 857000
  • 收稿日期:2024-12-26 出版日期:2025-11-20 发布日期:2025-11-17
  • 作者简介:杜军,正研级高级工程师,主要从事高原气候与气候变化、生态与农业气象等研究,E-mail:dujun0891@163.com
  • 基金资助:
    2024年西藏自治区重大科技专项(XZ202402ZD0006)

Spatio-temporal Variation Characteristics of Vapor Pressure Deficit and Its Causes in Xizang from 1981 to 2020 under the Background of Warming and Wetting

DU Jun, GAO Jia-jia, PHUNTSOKSAMTEN, SONAM, TASHIWANGLHA   

  1. 1.Xizang Institute of Plateau Atmospheric and Environmental Sciences/Xizang Open Laboratory for Plateau Atmospheric Environment, Lhasa 850001, China; 2. China Meteorological Adiministration Mêdog Field Science Experiment Base for Atmospheric Water Cycle/Mêdog National Climate Observatory/Xizang Mêdog Field Scientific Observation and Research Station for Atmospheric Water Cycle, Mêdog 860700; 3. Xizagê National Climate Observatory, China Meteorological Adiministration, Xizagê 857000
  • Received:2024-12-26 Online:2025-11-20 Published:2025-11-17

摘要:

饱和水汽压差(Vapor pressure deficitVPD)是表征大气干旱的一个重要变量,研究各地VPD时空变化特征对气候变化研究和农牧业生产等具有重要意义基于40a1981−2020年)西藏38个气象站点逐月平均气温、平均最高气温、平均最低气温、日照时数、降水量、相对湿度、水汽压和平均风速等地面气象资料,以及粮食产量、大气环流和海温等指数,采用线性倾向估计Pearson相关系数、Pettitt突变检验和逐步回归方法,分析近40a西藏饱和水汽压差时空变化特征及影响因子,以及对粮食产量的影响。结果表明:(1在空间上,西藏年平均VPD3个高值区,分别位于阿里西部、沿雅鲁藏布江河谷农区和怒江干热河谷的八宿;低值区分布在那曲市中东部和南部边缘地区。40a各站年VPD均趋于增大,增幅随海拔升高而变小。2在时间上,40a西藏年VPD以0.025kPa·10a−1的速率呈显著增大趋势,主要表现在秋、夏两季;且2005年前后年、季VPD发生突增现象。20世纪80年代和90年代年和季VPD均偏低,以90年代最明显;21世纪前10a春、秋季VPD偏低,夏、冬季VPD偏高,年VPD略偏高;21世纪10年代年、季VPD均偏高,主要表现在夏、秋季。(3除夏季外,季和年平均VPD与粮食产量尤其是单产呈显著正相关;生长季VPD与粮食总产呈显著正相关,其中4月和9VPD对粮食总产、单产的影响最显著VPD增大有利于粮食增产。(440a西藏四季和年平均气温升高是引起VPD增大的主导气象因子;影响年、季VPD变化的主导环流因子是西藏高原1指数,印度洋暖池面积指数是影响春、冬季VPD的主导海温因子,而热带印度洋全区一致海温模态指数却是影响夏、秋季和年VPD的主导海温因子,且主导因子在近40a呈极显著上升趋势,致使VPD明显增大。

关键词: 饱和水汽压差, 变化趋势, 突变, 粮食产量, 大气环流指数, 海温指数

Abstract:

Vapor pressure deficit (VPD) is an important parameter for featuring atmospheric drought, which plays a significant role in analyzing the impact of spatio−temporal VPD variations on the climate change and agricultural and animal husbandry production. The relevant monthly meteorological data, including mean air temperature(Tm), mean maximum air temperature, mean minimum air temperature, sunshine hours, precipitation, relative humidity, vapor pressure and mean wind speed, were collected at 38 meteorological stations in Xizang from 1981 to 2020. Several other relevant corresponding variables, such as the indices of grain yield, atmospheric circulation and sea surface temperature (SST), were also collected accordingly. Based on these materials, both the spatio−temporal characteristics of VPD variation and the influential factors were analyzed to identify their impacts on grain yield over Xizang in the recent 40 years, with the support of different statistical methods such as linear tendency estimation, Pearson's correlation coefficient, Pettitt mutation test method, linear tendency estimation and stepwise regression etc. The results indicated that: (1) spatially, there were 3 regions with high annual mean VPD in Xizang, which were located in the western part of Ngari district, the agricultural area along the Yarlung Zangbo river valley, and Baxoi station in the dry heat valley of the Nujiang river, respectively; the regions with low values were distributed in the east−central part of the Nagchu and at the southern edge of Xizang. In the recent 40 years, the annual VPD at all stations increased at varying rates of 0.014−0.064kPa·10y1 (13 stations P<0.01), with the largest value in Lhasa, followed by Xigazê (0.044kPa·10y1, P<0.001), and the smallest in Lhari. Overall, the linear trend of VPD decreased with the increase in altitude. (2) Temporally, the annual VPD in Xizang fluctuated greatly, showing a 'V' type change in the past 40 years. Initially, the VPD exhibited a significant decreasing trend from 1981 to 2000 at a rate of −0.020kPa·10y1 (P<0.05), then the VPD increased significantly with a rate of 0.053kPa·10y1 (P<0.01) from 2001 to 2020. Overall, the VDP showed an increasing trend of 0.025kPa·10y1 during 19812020. In addition, a sudden increase in both annual and seasonal VPD occurred around 2005. Both the annual and the seasonal VPD were lower in 1980s and 1990s, especially in the 1990s. In 2000s, the VPD showed lower values in spring and autumn, higher values in summer and winter, with slightly higher annual values. In contrast, both annual and seasonal values of VPD were higher in 2010s, especially in the summer and autumn times. (3) Except for the summer time, both seasonal and annual average VPD were positively correlated with grain yield significantly, especially with the yield per unit area in Xizang, which reached a very significant test level of P<0.001. The VPD in growing season was only positively correlated with total grain yield significantly, and VPD had the most significant effect on total yield and yield per unit area in April and September. The increase of VPD was beneficial to grain yield enhancement. In contrast, for maize and soybean cultivated in northeastern and northern China, crop yields decreased along with increasing VPD. Therefore, unlike other agricultural production regions in China, climate change might play a positive role in crop growth and yield formation through increasing VPD, meaning that water−saving technologies and agronomic management need to be strongly encouraged to adapt to the ongoing climate change in Xizang. (4) Different dominant factors were analyzed for meteorological, circulation and SST impacts on VDP variations over Xizang in the recent 40 years. The increase in seasonal and annual Tm was identified as the dominant factor for the meteorological impact, while the Xizang plateau region 1 index was determined to be the dominant circulation factor impacting annual and seasonal VPD variations. As for the dominant factors for SST impact, the Indian ocean warm pool area index was believed to be the dominant SST factor affecting VPD variations in spring and winter, while the Indian ocean basin−wide index was found to be the dominant SST factor affecting VPD variations in summer, autumn and all year around. All of the dominant factors mentioned above have shown a significant increasing trend in the last 40 years, resulting in a significant increase of VPD in Xizang accordingly.

Key words: Vapor pressure deficit, Linear trend, Climate mutation, Grain yield, Atmospheric circulation index, SST index