《山东大学学报(理学版)》 ›› 2026, Vol. 61 ›› Issue (10): 170-183.doi: 10.6040/j.issn.1671-9352.0.2026.003
• 水文过程与生态响应 • 上一篇
李爽1,2,李岩3,章四龙1,2*
LI Shuang1,2, LI Yan3, ZHANG Silong1,2*
摘要: 受全球变暖影响,黄河源区径流过程呈现复杂的时空响应。为揭示该区域未来气候与径流演变趋势,探究其河流生态流量风险,本研究基于CMIP6多模式集合数据驱动SWAT水文模型,模拟2025—2100年3种SSP情景下的未来径流变化;在此基础上,综合逐月次最小(大)值法、改进Tennant法与IHA-RVA法,确定生态流量阈值,并评估未来径流对于生态需水的满足程度。结果表明:(1)SWAT模型在黄河源区适用性良好(率定期与验证期NSE均大于0.8),偏差校正后的多模式集合数据能够可靠驱动径流模拟;(2)未来气候呈“暖湿化”趋势,降水波动增加,气温持续上升(最高、最低气温最大升幅分别达6.1 ℃、7.0 ℃);(3)未来径流量显著增加(增幅32.17%~58.26%),年内分布更趋集中,SSP2-4.5情景下年际波动最大;(4)未来生态需水保证率呈现显著季节差异,冬春季生态流量基本可保障,而夏秋季径流超过最大生态需水的比例显著升高(SSP5-8.5情景下部分月份超90%),预示汛期高流量生态风险加剧。研究结论可为区域水资源的合理配置与水生态保护提供科学依据。
中图分类号:
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