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利用谷歌地球引擎对一条无植被、短暂的河流洪水进行可视化:对快速环境变化时期河道-洪泛平原动态评估的启示。

Visualisation of flooding along an unvegetated, ephemeral river using Google Earth Engine: Implications for assessment of channel-floodplain dynamics in a time of rapid environmental change.

机构信息

Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan, 430074, China; Key Laboratory of Theory and Technology of Petroleum Exploration and Development in Hubei Province, Wuhan, 430074, China.

Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 3DB, UK.

出版信息

J Environ Manage. 2021 Jan 15;278(Pt 2):111559. doi: 10.1016/j.jenvman.2020.111559. Epub 2020 Nov 1.

Abstract

Given rapid environmental change, the development of new, data-driven, interdisciplinary approaches is essential for improving assessment and management of river systems, especially with respect to flooding. In the world's extensive drylands, difficulties in obtaining field observations of major hydrological events mean that remote sensing techniques are commonly used to map river floods and assess flood impacts. Such techniques, however, are dependent on available cloud-free imagery during or immediately after peak discharge, and single images may omit important flood-related hydrogeomorphological events. Here, we combine multiple Landsat images from Google Earth Engine (GEE) with precipitation datasets and high-resolution (<0.65 m) satellite imagery to visualise flooding and assess the associated channel-floodplain dynamics along a 25 km reach of the unvegetated, ephemeral Río Colorado, Bolivia. After cloud and shadow removal, Landsat surface reflectance data were used to calculate the Modified Normalized Difference Water Index (MNDWI) and map flood extents and patterns. From 2004 through 2016, annual flooding area along the narrow (<30 m), shallow (<1.7 m), fine-grained (dominantly silt/clay) channels was positively correlated (R = 0.83) with 2-day maximum precipitation totals. Rapid meander bend migration, bank erosion, and frequent overbank flooding was associated with formation of crevasse channels, splays, and headward-eroding channels, and with avulsion (shifting of flow from one channel to another). These processes demonstrate ongoing, widespread channel-floodplain dynamics despite low stream powers and cohesive sediments. Application of our study approaches to other dryland rivers will help generate comparative data on the controls, rates, patterns and timescales of channel-floodplain dynamics under scenarios of climate change and direct human impacts, with potential implications for improved river management.

摘要

鉴于环境的快速变化,开发新的、数据驱动的跨学科方法对于改进河流系统的评估和管理至关重要,特别是在洪水方面。在世界广大的干旱地区,获取主要水文事件实地观测数据的困难意味着遥感技术通常用于绘制河流洪水图并评估洪水影响。然而,这些技术依赖于峰值排放期间或之后立即可用的无云图像,并且单个图像可能会忽略重要的与洪水有关的水文地貌事件。在这里,我们结合来自 Google Earth Engine(GEE)的多个 Landsat 图像、降水数据集和高分辨率(<0.65 m)卫星图像,可视化洪水并评估玻利维亚裸露的、短暂的科罗拉多河 25 公里河段的相关河道-泛滥平原动态。在去除云和阴影之后,使用 Landsat 地表反射率数据来计算改进的归一化差异水体指数(MNDWI)并绘制洪水范围和模式。在 2004 年至 2016 年期间,狭窄(<30 m)、浅(<1.7 m)、细粒(主要为粉砂/粘土)河道的年度洪水面积与 2 天最大降水总量呈正相关(R=0.83)。快速弯道迁移、河岸侵蚀和频繁的漫滩洪水与冲沟、分流和溯源侵蚀河道的形成以及决口(水流从一条河道转移到另一条河道)有关。尽管水流功率和粘性沉积物较低,但这些过程仍表明存在广泛的河道-泛滥平原动态。将我们的研究方法应用于其他干旱地区的河流,将有助于生成关于在气候变化和直接人为影响情景下河道-泛滥平原动态的控制、速度、模式和时间尺度的比较数据,这可能对改善河流管理产生影响。

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