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Planform channel dynamics of the lower Colorado River: 1976-2000

机译:科罗拉多河下游的平面河道动力学:1976-2000年

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摘要

In the past two decades, major flood events have occurred on the lower Colorado River, a dramatic shift from the low flows and moderate floods associated with prior decades of river regulation. This study uses repeat aerial photography and Geographic Information System analysis to examine the planform channel response of the upper Colorado River delta (limitrophe reach) to this recently altered hydrology. Results indicate that channel contraction has been the dominant planform process in recent decades, but periodic floods resulted in channel expansion (1981-1988; 1997-2000) or likely reduced the channel contraction measured between successive aerial photographs (1976-1981; 1988-1994). Sinuosity adjustments were limited during the timeframe of the study (range: 1.31 to 1.38), but the channel did respond with large adjustments in channel width (range: 44 m to 355 m) and changes in total mid-channel bar area (range: 0 to 52.3 ha). A channel probability model developed for this study provides a raster image of the channel changes and depicts areas modified to varying degrees by flood flows. This historical study provides insight into how floods affect the channel system that provides the foundation for aquatic and riparian biodiversity. This issue is of increasing relevance given growing international interest in rehabilitating the riparian and aquatic ecosystems of the Colorado River delta through intentional flood flows.
机译:在过去的二十年中,科罗拉多河下游发生了重大洪水事件,这与先前几十年的河流管制相关的低流量和中等洪水发生了巨大变化。这项研究使用重复的航空摄影和地理信息系统分析来检查科罗拉多河上游三角洲(极限河段)对最近改变的水文学的平面通道响应。结果表明,近几十年来通道收缩一直是主要的平面过程,但是周期性的洪水导致通道扩张(1981-1988; 1997-2000),或者可能减少了连续航拍照片之间的通道收缩(1976-1981; 1988-1994) )。在研究的时间范围内,精确度调整是有限的(范围:1.31至1.38),但是通道确实对通道宽度(范围:44 m至355 m)进行了较大的调整,并且总的通道中间条形区域(范围: 0至52.3公顷)。为这项研究开发的通道概率模型提供了通道变化的光栅图像,并描述了因洪水而变化程度不同的区域。这项历史研究提供了有关洪水如何影响渠道系统的见识,洪水系统为水生和河岸生物多样性奠定了基础。鉴于国际上越来越有意通过有意的洪水来恢复科罗拉多河三角洲的河岸和水生生态系统,这一问题的相关性越来越高。

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