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Small-scale spatial variation of inundation dynamics in a floodplain of the Pantanal (Brazil)

机译:潘塔纳尔湿地(巴西)泛滥动力​​学的小范围空间变化

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The spatial and temporal variability of water levels was investigated across a section of floodplain in the Pantanal that represents typical geomorphic and ecological complexity of these environments. A series of 11 staff gauges were installed along a 12-km transect running perpendicularly from the Cuiabá River into the floodplain. The staff gauges were monitored fortnightly during the flood seasons from 2004 to 2007. Contrary to what is often assumed, the water surface profile was never level, and it was particularly variable when there was less water on the floodplain. Water surface slope varied from 1.4 × 10−4 (unitless) to 1.3 × 10−3 indicating substantial water movement that was verified by flow observations. The spatial patterns of water level variation were repeated across years, even though there was considerable interannual variation in magnitude and duration of floodplain inundation. In 2004 and 2005, the duration of inundation was 121 and 120 days, respectively, but in 2006 and 2007, inundation lasted 166 and 157 days, respectively. These observations reveal considerable small-scale spatial variability in the water surface profile, but with persistent patterns over space and time that are related to the river hydrograph and the channels that convey flood waters across the area. This study contributes to our understanding of inundation hydrology and its linkages to ecosystem processes, and additionally provides a valuable data set for calibration and validation of remote sensing approaches to measurement of inundation area and water movement across floodplains. Keywords Floodplain - River - Inundation - Pantanal - Hydrology - Geomorphology Handling editor: J. M. Melack
机译:在潘塔纳尔河泛滥平原的整个剖面上调查了水位的时空变化,这些剖面代表了这些环境的典型地貌和生态复杂性。沿着从Cuiabá河到洪泛区垂直延伸的12公里长的断面安装了一系列11个工作人员仪表。在2004年至2007年的汛期,每两周对工作人员的水位进行一次监测。与通常的假设相反,水面轮廓从未保持水平,当洪泛区的水量较少时,水面轮廓尤其可变。水面的倾斜度从1.4×10 −4 (无单位)变化到1.3×10 −3 (表明无水运动),已通过流量观测证实。尽管洪泛区淹没的规模和持续时间存在较大的年际变化,但多年以来,水位变化的空间模式一直在重复。在2004年和2005年,淹没持续时间分别为121天和120天,但在2006年和2007年,淹没持续时间分别为166天和157天。这些观察结果揭示了水面轮廓的小规模空间变化,但是在空间和时间上具有持续的模式,这与河流水文和将洪水输送到整个地区的河道有关。这项研究有助于我们对淹没水文学及其与生态系统过程的联系的理解,并且还提供了宝贵的数据集,可用于校准和验证测量洪泛区和淹没平原上的水流的遥感方法。洪泛区-河流-洪水-潘塔纳尔河-水文学-地貌学处理编辑:J. M. Melack

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