中国农业气象 ›› 2026, Vol. 47 ›› Issue (10): 1648-1657.doi: 10.3969/j.issn.1000-6362.2026.10.009

• 农业生物气象栏目 • 上一篇    下一篇

赤水河流域饱和水气压差时空变化特征及对仁怀市酒用高粱生产的影响

任青峰,谢璐繁,吴新豪,谢强,骆海顺   

  1. 贵州省仁怀市气象局,仁怀 564500
  • 收稿日期:2025-07-05 出版日期:2026-10-20 发布日期:2026-10-19
  • 作者简介:任青峰,高级工程师,研究方向为气候变化与应用气象,E-mail:jesusr@163.com
  • 基金资助:
    遵义市气象局市县联合基金项目(ZYQXKY−SX[2024]06号);贵州省气象局省市联合基金项目(黔气科合SS[2023]24号)

Spatiotemporal Evolution of Vapor Pressure Deficit in Chishui River Basin and Effects on Liquor−making Sorghum Prodution in Renhuai

REN Qing-feng, XIE Lu-fan, WU Xin-hao, XIE Qiang, LUO Hai-shun   

  1. Renhuai Meteorological Bureau of Guizhou Province, Renhuai 564500, China
  • Received:2025-07-05 Online:2026-10-20 Published:2026-10-19

摘要:

基于1981−2024年赤水河流域内10个国家气象站逐日资料,采用Tetens模型计算饱和水汽压差(Vapor pressure deficit,VPD),利用2006−2024年仁怀市逐年酒用高粱播种面积、产量和平均生育期数据,结合趋势分析、Mann–Kendall突变检验、小波分析等方法,探究赤水河流域VPD时空变化特征及对仁怀市酒用高粱生产的影响。结果表明:(1)1981−2024年赤水河流域年际、春季和夏季尺度VPD均呈极显著上升趋势(P<0.01),增速分别为0.005kPa·10a−1、0.007kPa·10a−1和0.007kPa·10a−1;冬季VPD显著增加(0.004kPa·10a−1,P<0.05),秋季变化趋势不显著;夏季变幅最大(0.105~0.207kPa),冬季变幅最小(0.074~0.124kPa);2001−2004年赤水河流域年际和各季节尺度VPD均发生集中突变后增加,且极端性随年代变化增强。(2)1981−2024年赤水河流域年际和各季节VPD均呈西北低−东南高的空间分布格局,未来3~7a赤水河流域年际和各季节VPD的变化特征可能持续加强。(3)2006−2024年仁怀市酒用高粱生育期(4−8月)平均VPD每增加0.01kPa,单位面积产量下降108.8kg·hm−2;VPD增加既对酒用高粱产量产生直接负影响,又通过放大平均气温、空气相对湿度的协同胁迫间接加剧减产。建议通过提高土壤保水、增加灌溉设施等措施,缓和VPD升高对仁怀酒用高粱生产的风险。

关键词: 赤水河流域, 干湿变化, 相对湿度, 酒用高粱, 气候变化

Abstract:

Based on daily observational data from ten national meteorological stations in the Chishui River basin (1981–2024) , the vapor pressure deficit (VPD) was calculated using the Tetens formula. To assess the effect, annual data on sowing area, yield and the long−term average growth period of liquor−making sorghum in Renhuai (2006–2024) were utilized. The temporal–spatial characteristics of VPD were analyzed using trend analysis, Mann–Kendall test and wavelet analysis, followed by a quantitative assessment of the VPD−induced stress on liquor−making sorghum production in Renhuai. The results showed that: (1) from 1981 to 2024, the VPD in the Chishui River basin exhibited a highly significant increasing trend at the annual, spring and summer scales (P<0.01), with rates of 0.005kPa·10y−1, 0.007kPa·10y−1 and 0.007kPa·10y−1, respectively. A significant increase was also observed in winter (0.004kPa·10y−1, P<0.05), while the autumn trend was not significant. The greatest change occurred in summer (0.105 to 0.207kPa), and the smallest in winter (0.074 to 0.124kPa). Following an abrupt change observed from 2001 to 2004 across annual and seasonal scales, the VPD showed a consistent increase, and its variability increased over the subsequent decades. (2) From 1981 to 2024, annual and seasonal VPD consistently showed a spatial pattern of low in the northwest and high in the southeast. This pattern was projected to strengthen over the next 3–7 years of annual and seasonal VPD in the Chishui River basin. (3) During the period of 2006–2024, every 0.01kPa increase in the mean VPD of the liquor−making sorghum growing season (April–August) in Renhuai reduced the yield by 108.8kg·ha−1. The increase of VPD had a direct negative effect on the yield and indirectly amplified the yield loss by intensifying the combined stresses of air temperature and relative humidity. Soil−water conservation and irrigation infrastructure are recommended to mitigate the risks associated with rising VPD.

Key words: the Chishui River basin, Dry?wet evolution, Relative humidity, Liquor?making sorghum, Climate change