干旱区研究 ›› 2024, Vol. 41 ›› Issue (12): 2045-2055.doi: 10.13866/j.azr.2024.12.07 cstr: 32277.14.AZR.20241207

• 水土资源 • 上一篇    下一篇

气候变化下泾河流域蓝绿水变化趋势及预测

张嘉琪1,2,3(), 刘招1,2,3(), 韩忠青1,2,3, 王丽霞4, 张晋霞1,2,3, 岳甲寅1,2,3, 管子隆5   

  1. 1.长安大学水利与环境学院,陕西 西安 710054
    2.长安大学旱区地下水文与生态效应教育部重点实验室,陕西 西安 710054
    3.长安大学水利部旱区生态水文与水安全重点实验室,陕西 西安 710054
    4.长安大学地质工程与测绘学院,陕西 西安 710054
    5.中国电建集团西北勘测设计研究院有限公司,陕西 西安 710065
  • 收稿日期:2024-04-21 修回日期:2024-09-21 出版日期:2024-12-15 发布日期:2024-12-20
  • 通讯作者: 刘招. E-mail: lz975@163.com
  • 作者简介:张嘉琪(2001-),女,博士研究生,主要从事水文学及水资源研究. E-mail: zjq18991324073@163.com
  • 基金资助:
    陕西省自然科学基础研究计划(2023-JC-QN-0372);国家自然科学基金(42207084)

Trend change and prediction of blue-green water in the Jinghe River Basin under climate change

ZHANG Jiaqi1,2,3(), LIU Zhao1,2,3(), HAN Zhongqing1,2,3, WANG Lixia4, ZHANG Jinxia1,2,3, YUE Jiayin1,2,3, GUAN Zilong5   

  1. 1. School of Water and Environment, Chang’an University, Xi’an 710054, Shaanxi, China
    2. Key Laboratory of Subsurface Hydrology and Ecological Effect in Arid Region of the Ministry of Education, Chang’an University, Xi’an 710054, Shaanxi, China
    3. Key Laboratory of Eco-hydrology and Water Security in Arid and Semi-arid Regions of Ministry of Water Resources, Chang’an University, Xi’an 710054, Shaanxi, China
    4. College of Geological Engineering and Geomatics, Chang’an University, Xi’an 710054, Shaanxi, China
    5. Powerchina Northwest Engineering Corporation Limited, Xi’an 710065, Shaanxi, China
  • Received:2024-04-21 Revised:2024-09-21 Published:2024-12-15 Online:2024-12-20

摘要:

基于泾河流域1980—2020年气象站点实测数据、水文站点实测径流数据及CMIP6未来气候模式,通过Delta降尺度的方法处理CMIP6气候数据,耦合SWAT(Soil and Water Assessment Tool)水文模型,探究流域内气候变化下蓝绿水的变化特征。结果表明:在SSP1-2.6路径下,研究区的蓝绿水量均呈现不显著上升趋势,在SSP3-7.0路径下,研究区蓝水量为不显著下降趋势,绿水量为显著上升趋势;在SSP5-8.5路径下,蓝水量为不显著下降趋势,绿水量为不显著上升趋势。3种路径下的多年平均蓝水量均较历史时期有所减小,多年平均蓝水量分别为128.8 mm、117.2 mm、126 mm,多年平均绿水量都有所增加,绿水量分别为372.7 mm、369.3 mm、372.1 mm,并且绿水系数均大于历史时期。蓝绿水空间分布特征均为从西北向东南地区递增,各路径之间蓝绿水的空间分布特征基本完全相同。

关键词: SWAT模型, Delta降尺度, 气候变化, CMIP6气候模式, 蓝绿水, 泾河流域

Abstract:

In this study, we analyzed meteorological data from 1980 to 2020, hydrological runoff data, and future climate models from CMIP6 in the Jinghe River Basin. The CMIP6 climate data was processed using the delta downscaling method and coupled with the Soil and Water Assessment Tool hydrological model to investigate the variations in blue-green water due to climate change in the basin. The results showed that under the SSP1-2.6 pathway, the blue-green water content in the study area exhibited an insignificant upward trend. Under the SSP3-7.0 pathway, the blue water content showed an insignificant downward trend, while the green water content showed a significant upward trend. Similarly, under the SSP5-8.5 pathway, the blue water content showed an insignificant downward trend, and the green water content also exhibited an insignificant upward trend. The average annual blue water volume under the three pathways decreased compared to the historical period, with annual averages of 128.8 mm, 117.2 mm, and 126 mm, respectively. Conversely, the average annual green water volume increased, recording values of 372.7 mm, 369.3 mm, and 372.1 mm, resulting in a green water coefficient higher than that of the historical period. The spatial distribution of blue-green water increased from northwest to southeast, with consistent spatial distribution characteristics across each pathway.

Key words: SWAT model, Delta downscaling, climate change, CMIP6 climate model, blue-green water, Jinghe River Basin