On river‐floodplain interaction and hydrograph skewness. Issue 10 (4th October 2016)

• Record Type: Journal Article
• Authors: Fleischmann, Ayan S.; Paiva, Rodrigo C. D.; Collischonn, Walter; Sorribas, Mino V.; Pontes, Paulo R. M.
• Is Part Of: Water resources research. Volume 52:Issue 10(2016:Oct.)
• Page Start: 7615
• Page End: 7630
• Publication Date: 2016-10-04
• Subjects: river‐floodplain interaction -- hydrograph shape -- flood wave celerity; Hydrology -- Periodicals; 333.91
• DOI: 10.1002/2016WR019233
• Languages: English
• ISSNs: 0043-1397

Abstract

Abstract: Understanding hydrological processes occurring within a basin by looking at its outlet hydrograph can improve and foster comprehension of ungauged regions. In this context, we present an extensive examination of the roles that floodplains play on driving hydrograph shapes. Observations of many river hydrographs with large floodplain influence are carried out and indicate that a negative skewness of the hydrographs is present among many of them. Through a series of numerical experiments and analytical reasoning, we show how the relationship between flood wave celerity and discharge in such systems is responsible for determining the hydrograph shapes. The more water inundates the floodplains upstream of the observed point, the more negatively skewed is the observed hydrograph. A case study is performed in the Amazon River Basin, where major rivers with large floodplain attenuation (e.g., Purus, Madeira, and Juruá) are identified with higher negative skewness in the respective hydrographs. Finally, different wetland types could be distinguished by using this feature, e.g., wetlands maintained by endogenous processes, from wetlands governed by overbank flow (along river floodplains). A metric of hydrograph skewness was developed to quantify this effect, based on the time derivative of discharge. Together with the skewness concept, it may be used in other studies concerning the relevance of floodplain attenuation in large, ungauged rivers, where remote sensing data (e.g., satellite altimetry) can be very useful. Key Points: River‐floodplain interaction causes negative skewed hydrographs Inverse relationship between flood wave celerity and discharge leads to negative skewness Potential to characterize wetland types using river hydrograph shape