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Spatial and temporal dynamics of river channel migration and vegetation in central Amazonian white-water floodplains by remote-sensing techniques

机译:遥感技术在亚马逊河中部白水漫滩中河道迁移和植被的时空动态

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We investigated spatial and temporal migration of the Solimoes, the Japura, and the Aranapu River channels in western Brazilian Amazonia with Landsat TM imagery over a 21-year period. Additionally. we classified band monitored how channel migrations affect the distribution of pioneer vegetation and old-growth forest. The cloud-free study area was 153,032 ha - open water plus 3 km inland on each margin. The channel migration rates, expressed as percent dislocation of the open water body of the river year(-1), were lowest in the Japura River (1.2%), and highest in the Aranapu channel (2.5%), the point bars at river confluence being the most affected landforms subject to geomorphic changes. Annual rates of lateral erosion and accretion of vegetated land along the three rivers were well-balanced. They averaged 0.79 and 0.83% of the cloud-free channel area over the 21 years. The Solimoes River was more dynamic than the Japura River, which can be traced to higher water discharge and sediment load. During the 21 years, the area covered by pioneer vegetation increased by 5.8% of the study area, while late-succession areas decreased by a similar amount (5.5%). According to local biomass estimates of the different vegetation types, these values suggest that C-releases by alluvial erosion would be much higher than C-sequestration caused by the creation of areas suitable for colonization by pioneer vegetation at our study site.
机译:我们用Landsat TM影像调查了巴西西部亚马逊地区Solimoes,Japura和Aranapu河河道的时空迁移,历时21年。另外。我们对频段进行了分类监控,以了解渠道迁移如何影响先锋植被和旧林的分布。无云研究区域面积为153,032公顷-开放水域,每个边缘带3公里内陆。河道迁移率以河年开放水体的位错百分比表示(-1),在Japura河中最低(1.2%),在Aranapu河道中最高(2.5%),这是河中的点交汇处是受地貌变化影响最大的地貌。沿这三条河的横向侵蚀和植被的年积速率是均衡的。在过去21年中,它们平均占无云通道面积的0.79%和0.83%。 Solimoes河比Japura河更具活力,这可以追溯到较高的排水量和泥沙量。在21年中,先驱植被覆盖的面积增加了研究面积的5.8%,而后继面积减少了类似数量(5.5%)。根据当地对不同植被类型的生物量估计,这些值表明,冲积侵蚀引起的碳释放量将远远高于在我们的研究地点创建的适于先锋植物定殖的区域引起的碳固存。

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