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蒙古高原生态干旱监测及时空变化OA

Ecological drought monitoring and spatiotemporal changes in the Mongolian Plateau

中文摘要英文摘要

在全球气候变暖加剧的背景下,蒙古高原作为生态脆弱区面临日益严峻的干旱威胁.为量化干旱对生态系统的影响,基于气象与遥感数据计算标准化生态缺水指数(SEWDI),系统评估其在蒙古高原生态干旱监测中的适用性,揭示1982-2022年蒙古高原生态干旱的时空演变规律,并利用游程理论提取生态干旱特征.结果表明:(1)SEWDI在时空尺度上与植被指标的相关性优于标准化降水蒸散指数(SPEI)、标准化降水指数(SPI)和自校正帕尔默干旱严重度指数(ScPDSI),表现出更强的生态干旱表征能力.(2)近40 a来,蒙古高原生态干旱以-0.0168·a-1呈显著加剧趋势,空间上干旱化趋势集中于北部,蒙古国干旱程度整体高于中国内蒙古自治区;季节上,夏季干旱加剧最为明显,春秋次之,冬季则略有缓解.(3)游程理论分析表明,蒙古高原生态干旱烈度北高南低,历时北长南短,频率北低南高,强度则西北低东南高.SEWDI通过整合植被需水与耗水动态,显著提升了生态干旱监测的敏感性与准确性,可为区域差异化抗旱与生态管理策略提供科学依据与技术支撑.

The Mongolian Plateau is an ecologically vulnerable region that is susceptible to increasingly severe drought threats due to intensifying global warming.To quantify the impact of drought on ecosystems,the stan-dardized ecological water deficit index(SEWDI)was calculated based on meteorological and remote sensing da-ta.This study systematically evaluated the application of the SEWDI in monitoring ecological drought on the Mongolian Plateau.It revealed the spatiotemporal evolution patterns of ecological drought from 1982 to 2022 and extracted ecological drought characteristics using run theory.The results of the study indicate that:(1)SEW-DI demonstrates stronger correlations with vegetation indices across temporal and spatial dimensions than tradi-tional drought indices,including the standardized precipitation evapotranspiration index,the standardized precipi-tation index,and the self-calibrating Palmer drought severity index.These findings suggest that SEWDI exhibits superior capability in characterizing ecological drought.(2)Over the past 40 years,ecological drought has intensi-fied significantly at a rate of-0.0168·a-1.The drying trend has been primarily concentrated in the northern re-gions,and the conditions have been more severe in Mongolia than in China's Inner Mongolia Autonomous Re-gion.The severity of drought conditions exhibited seasonal patterns,with the most pronounced exacerbation oc-curring during the summer months,followed by a notable intensification in spring and autumn.Conversely,a mar-ginal alleviation was observed during the winter season.(3)The ecological drought severity in the Mongolian Pla-teau is higher in the northern regions and lower in the southern regions.Furthermore,the duration of drought is prolonged in the northern regions and is comparatively reduced in the southern regions.The frequency is lower in the north and higher in the south,whereas the intensity is lower in the northwest and higher in the southeast.SEWDI has been shown to enhance the sensitivity and accuracy of ecological drought monitoring by integrating vegetation water demand and consumption dynamics.This integration provides a scientific basis for region-spe-cific drought resistance and ecological management strategies.

温明君;武志涛;杜自强;梁寒雪;陈鑫;雷添杰

山西大学黄土高原研究所,山西 太原 030006山西大学黄土高原研究所,山西 太原 030006山西大学黄土高原研究所,山西 太原 030006山西大学黄土高原研究所,山西 太原 030006山西大学黄土高原研究所,山西 太原 030006中国农业科学院农业环境与可持续发展研究所,北京 100081

生态干旱干旱演变游程理论蒙古高原

ecological droughtdrought evolutionrun theoryMongolian Plateau

《干旱区地理》 2026 (7)

1311-1322,12

国家重点研发计划课题(2023YFF1305102)国家自然科学基金(41977412)山西省科技创新人才团队项目(202204051001010)资助

10.12118/j.issn.1000-6060.2025.489

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