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Regional assessment of the multi-decadal changes in braided riverscapes following large floods (Example of 12 reaches in South East of France)

机译:大洪水后辫状河景多年代际变化的区域评估(以法国东南部的12个河段为例)

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The district of the France Rh?ne basin is characterised by severalbraided reaches, preserved from the widespread disappearing occurred in the20th century. Even if the overall pattern is evolving through a generalriver narrowing, some reaches have shown to be still active and havewidened. The preliminary results suggest that differences in width patterncould be related to several factors, such as high magnitude and lowfrequency floods, and geographical position in the catchment whichinfluences bedload delivery conditions and vegetation recruitment related toclimate. From an initial set of 53 braided reaches, we selected 12 sites,distributed into four main hydro-geographical regions. Reaches were selectedto be representative of the overall study area. We analysed the braidingwidth pattern and the vegetation pattern dynamic among five observationperiods dating from the 1950s to the 2000s. We hypothesised that acomparative analysis of a detailed temporal trajectory (i.e. five dates) ofa set of rivers within several hydro-geographical contexts would allow us tobetter distinguish the relative role of floods (in terms of magnitude andduration) and other controlling factors acting at the regional scale. Weshowed that active channel width is controlled mainly by Q10 flood andsecondarily by bedload availability whereas island pattern is in large partindependent of flood series characters. Moreover a clear regionaldifferentiation, constant over time, in terms of riverscape response isobserved, mainly opposing south-western and south-eastern reaches. Thisopposition depends on several concurring factors, i.e. the flood characters,the river activity, the human influence and the climate. Finally, thesefindings allowed us to highlight those sectors in which the braided patterncould disappear, and those sectors in which the braided pattern is stillactive, because critical processes responsible of channel dynamic are stillpresent.
机译:法国罗纳河盆地地区以几个辫状河段为特征,并保留了20世纪大范围消失的趋势。即使总体格局正在通过一般河道的缩小而演变,但有些河段仍显示出活跃并扩大了。初步结果表明,宽度格局的差异可能与若干因素有关,例如高强度和低频洪水,以及流域中的地理位置,这些都影响着与气候有关的基床输送条件和植被的吸收。在最初的53条辫状河段中,我们选择了12个地点,分布在四个主要的水文地理区域。选择研究范围以代表整个研究领域。我们分析了1950年代至2000年代的5个观测期的辫带宽度格局和植被格局动态。我们假设,对几种水文地理环境中的一组河流的详细时间轨迹(即五个日期)进行比较分析,将使我们能够更好地区分洪水的相对作用(就强度和持续时间而言)和其他作用于区域的控制因素规模。研究表明,主动河道宽度主要由 Q 10 洪水控制,其次由河床承载力控制,而岛型在很大程度上与洪水序列特征无关。此外,在河流景观响应方面观察到明显的区域差异,随时间变化是恒定的,主要是与西南和东南方向相对。这种反对取决于几个共同的因素,即洪水特征,河流活动,人类影响和气候。最后,这些发现使我们能够突出显示那些可能会消失的编织模式的扇区,以及那些仍然处于编织模式的扇区,因为仍然存在负责通道动态的关键过程。

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