干旱区地理 ›› 2026, Vol. 49 ›› Issue (8): 1572-1586.doi: 10.12118/j.issn.1000-6060.2025.696 cstr: 32274.14.ALG2025696
闫鹏旭1(
), 张丽华1,2(
), 曾繁星3, 拜小辉1, 叶阳1, 曹轶杰1
收稿日期:2025-10-29
修回日期:2025-11-24
出版日期:2026-08-25
发布日期:2026-08-21
通讯作者:
张丽华(1980-),女,博士,副教授,主要从事气候变化下的生态响应研究. E-mail: zhanglihualz@126.com作者简介:闫鹏旭(2004-),男,本科生,主要从事自然地理学研究. E-mail: ypengxuy@163.com
基金资助:
YAN Pengxu1(
), ZHANG Lihua1,2(
), ZENG Fanxing3, BAI Xiaohui1, YE Yang1, CAO Yijie1
Received:2025-10-29
Revised:2025-11-24
Published:2026-08-25
Online:2026-08-21
摘要:
青海湖流域是青藏高原东北缘典型的高寒山地内流河流域,研究其水碳耦合机制对揭示高寒生态系统碳水交互规律、支撑水资源与碳汇协同管理具有重要意义。基于2000—2024年多源遥感与气象数据,以净初级生产力(NPP)、蒸散发(ET)和水分利用效率(WUE)为核心变量,系统分析其时空变化特征,并融合随机森林与XGBoost双机器学习方法,从空间与时间双维度解析驱动机制。结果表明:(1) 时间变化上,近25 a流域NPP与ET均呈显著上升趋势,增速分别为2.511 g C·m-2·a-1、4.470 mm·a-1,WUE以2017年为转折点呈先降后升的非线性变化。(2) 空间分布上,NPP与WUE呈“东南高、西北低”格局,ET呈“北高南低”分布,空间异质性显著。(3) 空间尺度上,海拔显著控制NPP与WUE的空间分异,对ET无显著影响;植被类型主导NPP与WUE空间差异,沼泽、栽培植被、草原及灌丛的固碳能力与水分利用效率更高;气温与叶面积指数(LAI)对NPP呈显著正向驱动,降水量与气温共同调控ET,WUE与降水量呈显著负相关。(4) 时间尺度上,LAI是NPP变化的核心驱动因子(RF特征重要性0.467,XGBoost为0.337),ET受LAI与降水协同调控,WUE对降水量、水体面积等水分条件更为敏感,模型解释难度显著高于单一水碳变量。研究结果揭示了高寒内流河流域水碳耦合的时空尺度驱动规律,可为青藏高原生态保护与水碳资源综合管理提供科学依据。
闫鹏旭, 张丽华, 曾繁星, 拜小辉, 叶阳, 曹轶杰. 青海湖流域近25 a水碳变量时空变化与影响因素[J]. 干旱区地理, 2026, 49(8): 1572-1586.
YAN Pengxu, ZHANG Lihua, ZENG Fanxing, BAI Xiaohui, YE Yang, CAO Yijie. Spatiotemporal changes and influencing factors of water and carbon variables in the Qinghai Lake Basin over the past 25 years[J]. Arid Land Geography, 2026, 49(8): 1572-1586.
表2
数据信息与来源"
| 数据 | 单位 | 空间分辨率 | 数据来源 | 年份 |
|---|---|---|---|---|
| 净初级生 产力(NPP) | g C·m-2 | 500 m | MOD17A3 | 2000—2024 |
| 蒸散发(ET) | mm | 500 m | MOD16A3 | 2000—2024 |
| 海拔高度 | m | 30 m | ASTER GDEM V3 | - |
| 植被类型 | - | 1 km | 中国1:1000000 植被数据集 | 2023 |
| 气温 | ℃ | 1 km | ERA5-Land再分析数据集 | 2000—2024 |
| 降水量 | mm | 1 km | ERA5-Land 再分析数据集 | 2000—2024 |
| 太阳辐射 | MJ·m-2 | 1 km | ERA5-Land 再分析数据集 | 2000—2024 |
| 风速 | m·s-1 | 0.01° | 中国0.01°分辨率 逐年风速栅格数据 | 2000—2024 |
| 叶面积指数(LAI) | - | 500 m | MOD15A2 | 2000—2024 |
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