干旱区地理 ›› 2024, Vol. 47 ›› Issue (8): 1314-1326.doi: 10.12118/j.issn.1000-6060.2023.404
古丽扎尔·莫明1,2(), 杨莲梅2(), 刘艳2, 李新国1
收稿日期:
2023-08-05
修回日期:
2023-10-07
出版日期:
2024-08-25
发布日期:
2024-09-02
通讯作者:
杨莲梅(1969-),女,博士,研究员,主要从事天气气候和云降水物理研究. E-mail: yanglm@idm.cn作者简介:
古丽扎尔·莫明(1998-),女,硕士研究生,主要从事空间信息分析与应用研究. E-mail: gz2233711745@163.com
基金资助:
Gulzar MOMIN1,2(), YANG Lianmei2(), LIU Yan2, LI Xinguo1
Received:
2023-08-05
Revised:
2023-10-07
Published:
2024-08-25
Online:
2024-09-02
摘要:
基于1990—2022年伊犁河流域洪水灾情数据集,结合高程、归一化植被指数等孕灾环境因子,研究伊犁河流域洪水灾害时空分布及孕灾环境特征,并分析洪水灾害发生规律和孕灾环境之间的联系。结果表明:(1) 研究区洪水灾害可分为3种:暴雨洪水、融雪洪水和混合洪水(暴雨加融雪造成洪水),其中,暴雨洪水灾害最多(占80.0%)、融雪洪水灾害最少(占3.4%);洪水灾害呈流域北部多于南部、东段多于西段的空间分布,尼勒克县最多、霍尔果斯市最少。(2) 近30 a来洪水灾害频次呈年际和年代际增多趋势,洪水灾害年均约11.6次·a-1,2010年最多(43次),2000—2011年最多(149次)。洪水灾害在夏季最多,春季次之,秋季最少,6月最多(年均3.3次·a-1),10月最少(年均0.06次·a-1),其中暴雨洪水灾害夏季最多,年均9.3次·a-1,6月最多(110次),10月最少(2次),混合洪水灾害春多夏少,3月最多(36次),7月最少(8次),年均1.9次·a-1,融雪洪水灾害3月最多(12次),只发生于春季,年均0.4次·a-1。(3) 孕灾环境敏感性等级综合分布显示,灾害发生过程中,各孕灾因子共同起作用,影响洪水灾害的空间分布和强度。尼勒克县、特克斯县、新源县、昭苏县和霍尔果斯市境内的极高敏感区域分布较多。结合洪水灾害时空分布和孕灾环境等级综合分布可知,洪水灾害多发生在极高敏感区和高敏感区分布较多的流域东段和北部区域。
古丽扎尔·莫明, 杨莲梅, 刘艳, 李新国. 伊犁河流域近30 a洪水灾害时空分布及孕灾环境特征研究[J]. 干旱区地理, 2024, 47(8): 1314-1326.
Gulzar MOMIN, YANG Lianmei, LIU Yan, LI Xinguo. Spatial and temporal distribution of flood disasters and characteristics of disaster-prone environment in Ili River Basin in recent 30 years[J]. Arid Land Geography, 2024, 47(8): 1314-1326.
表6
伊犁河流域孕灾环境敏感性评价指标体系"
指标层 | 极低敏感 | 低敏感 | 中敏感 | 高敏感 | 极高敏感 | 权重 |
---|---|---|---|---|---|---|
高程/m | <1500 | 1501~2000 | 2001~2500 | 2501~3000 | 3001~6231 | 0.28 |
坡度/(°) | <8 | 9~18 | 19~28 | 29~38 | 39~85 | 0.10 |
地表粗糙度/(°) | <1.04 | 1.05~1.21 | 1.22~1.48 | 1.49~1.93 | >1.94 | 0.05 |
水域缓冲区/km | >15 | 9~15 | 6~9 | 3~6 | <3 | 0.33 |
NDVI | >0.8 | 0.6~0.8 | 0.4~0.6 | 0.2~0.4 | <0.2 | 0.11 |
土地利用类型 | 建设用地 | 林地 | 耕地、草地 | 未利用地 | 水域 | 0.13 |
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