复杂地形区地表蒸散量遥感反演研究——以海河流域为例
批准号:
42101040
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
刘兴冉
依托单位:
学科分类:
水文学和气候学
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
刘兴冉
中文摘要
复杂地形区地表蒸散量的估算是水文学相关领域研究的热点与难点之一。近年来海河流域山区植被覆盖增加迅速,植被变化引起的水循环变化对于流域水资源的形成至关重要,准确估算山区蒸散耗水对于科学评估该区域水文循环变化以及对水资源的影响意义重大。然而,海河流域山区地形复杂,观测资料稀少,如何准确估算山区蒸散成为该区域水文研究和水资源管理必须解决的技术瓶颈。因此,本项目以海河流域为例,基于遥感数据、气象数据与地形数据改进复杂地形区关键陆面参数的估算方法,实现地形对地表辐射通量、热通量的再分配,建立既简单实用又能刻画复杂地形区地表通量过程主要特征的蒸散发模型,并通过优化时间尺度扩展方法反演过去30年海河流域地表蒸散时空分布,探究复杂地形下地表蒸散量的关键影响因素。研究结果可为复杂地形区径流的预测和水资源的合理利用提供理论指导,并为海河流域日益短缺的水资源问题提供决策依据。
英文摘要
Estimation of surface evapotranspiration in complex terrain is one of the hot and difficult issues in hydrology. Vegetation fraction cover on the mountainous area has increased rapidly in Haihe river basin in recent years. Water cycle change in the mountainous areas caused by vegetation change is of great importance to the formation of water resources in the basin. Estimate evapotranspiration accurately in the mountainous area is of great significance for scientific evaluation of the change in water cycle and the impact on water resources in this region. However, the mountainous area of the Haihe River Basin is characterized by complex terrain and scarce observation data. How to accurately estimate the evapotranspiration in the mountainous area has become a technical bottleneck that must be solved for hydrological research and water resources management in this region. Therefore, this project aims to take the Haihe River Basin as an example, improve the estimation method of the key parameters in complex terrain based on remote sensing data, meteorological data and topographic data, realize the redistribution of surface radiation flux and heat flux by terrain, establish a simple and practical evapotranspiration model that can describe the main characteristics of surface flux process in complex terrain, and obtain the spatial and temporal distribution of evapotranspiration in the Haihe River Basin in the past 30 years by optimizing temporal extrapolation methods, and explore the key influencing factors of surface evapotranspiration in complex terrain. The results can provide theoretical guidance for the prediction of runoff and rational utilization of water resources in complex terrain, and provide decision-making basis for the problem of water resources shortage in Haihe River Basin.
地表蒸散是土壤-植被-大气系统中水分循环与热量传输的重要环节,是水量平衡与能量平衡的重要组成部分,影响着大气圈-水圈-生物圈的物质转化与能量循环,是水循环中最难测算的分量。复杂地形区蒸散量受下垫面地形、植被、温度、湿度等多方面的影响,如何准确模拟区域地表蒸散,尤其是在地形复杂的山区,是该领域研究的热点与难点所在。本项目以海河流域为例,基于遥感数据、地形数据及气象数据,考虑复杂下垫面对地表各辐射通量等关键陆面参数的影响,改进了遥感蒸散发模型在复杂地形区的应用,建立了相对精确且易于在复杂地形应用的蒸散发模型,并通过时间尺度扩展获取了近30年海河流域地表蒸散量的时空分布,探究了复杂地形下地表蒸散量的关键影响因素。模型改进方面主要表现在:综合考虑了大气、下垫面及地形的影响,从直接辐射、天空散射辐射及周围地形反射辐射三方面对海河流域太阳短波辐射进行估算,并创造性地运用遥感数据反演气象数据空间分布,弥补了气象数据空间插值的不足,修正了净长波辐射计算公式中的参数,使地表辐射平衡项结果精确性得到了较大提升。在土壤水分的遥感反演方面将适用于平原地区的TTME模型成功运用至山区地表,避免了人为选取极值点所带来的误差。研究结果发现,海河流域近30年地表蒸散量呈现上升趋势,月蒸散量年内呈现“单峰”变化趋势,季节性差异特征明显,夏季最大,春秋次之,冬季最小。海河流域蒸散量受地形、气候、土地覆被变化的影响均显著,但受地形影响最大,其次为气温,受植被覆盖度的影响最小。研究结果对于科学评估海河流域水文循环变化以及对水资源具有重要意义,所建立的复杂地形区遥感蒸散发模型也可推广应用于其他复杂地形区,为其他地区水热通量模拟提供借鉴。
国内基金
海外基金