Extreme flood‐driven fluvial bank erosion and sediment loads: direct process measurements using integrated Mobile Laser Scanning (MLS) and hydro‐acoustic techniques

ABSTRACT: This methods paper details the first attempt at monitoring bank erosion, flow and suspended sediment at a site during flooding on the Mekong River induced by the passage of tropical cyclones. We deployed integrated mobile laser scanning (MLS) and multibeam echo sounding (MBES), alongside acoustic Doppler current profiling (aDcp), to directly measure changes in river bank and bed at high (˜0.05 m) spatial resolution, in conjunction with measurements of flow and suspended sediment dynamics. We outline the methodological steps used to collect and process this complex point cloud data, and detail the procedures used to process and calibrate the aDcp flow and sediment flux data. A comparison with conventional remote sensing methods of estimating bank erosion, using aerial images and Landsat imagery, reveals that traditional techniques are error prone at the high temporal resolutions required to quantify the patterns and volumes of bank erosion induced by the passage of individual flood events. Our analysis reveals the importance of cyclone‐driven flood events in causing high rates of erosion and suspended sediment transport, with a c. twofold increase in bank erosion volumes and a fourfold increase in suspended sediment volumes in the cyclone‐affected wet season. Copyright © 2016 John Wiley & Sons, Ltd.

[1]  Juha Hyyppä,et al.  Morphological changes on meander point bars associated with flow structure at different discharges , 2013 .

[2]  J. O’Connor,et al.  Geomorphically Effective Floods , 2013 .

[3]  C. Delacourt,et al.  Very high spatial resolution imagery for channel bathymetry and topography from an unmanned mapping controlled platform , 2007 .

[4]  A. Ito,et al.  Development of a meandering channel caused by the planform shape of the river bank , 2013 .

[5]  M. Bauer,et al.  Airborne laser scanning for riverbank erosion assessment , 2005 .

[6]  Nick J. Mount,et al.  Evolutionary, multi-scale analysis of river bank line retreat using continuous wavelet transforms: Jamuna River, Bangladesh , 2013 .

[7]  B. Calder,et al.  Automatic processing of high‐rate, high‐density multibeam echosounder data , 2003 .

[8]  Daniel R. Parsons,et al.  Comparison of fixed- and moving-vessel flow measurements with an aDp in a large river , 2007 .

[9]  M. Kummu,et al.  A physically based model to predict hydraulic erosion of fine-grained riverbanks: The role of form roughness in limiting erosion , 2010 .

[10]  S. Darby,et al.  Modulation of outer bank erosion by slump blocks: Disentangling the protective and destructive role of failed material on the three‐dimensional flow structure , 2015 .

[11]  J. Brasington,et al.  Modeling river bed morphology, roughness, and surface sedimentology using high resolution terrestrial laser scanning , 2012 .

[12]  Qiuwen Chen,et al.  Flow separation at the inner (convex) and outer (concave) banks of constant‐width and widening open‐channel bends , 2013 .

[13]  L. James,et al.  Geomorphic and Sedimentological Controls on the Effectiveness of an Extreme Flood , 1998, The Journal of Geology.

[14]  J. Hyyppä,et al.  Application of boat‐based laser scanning for river survey , 2009 .

[15]  F. Magilligan Thresholds and the spatial variability of flood power during extreme floods , 1992 .

[16]  C. Renshaw,et al.  The efficacy of stream power and flow duration on geomorphic responses to catastrophic flooding , 2015 .

[17]  V. Kale Geomorphic effectiveness of extraordinary floods on three large rivers of the Indian Peninsula , 2007 .

[18]  S. Lane,et al.  Causes of rapid mixing at a junction of two large rivers: Río Paraná and Río Paraguay, Argentina , 2008 .

[19]  S. Lane,et al.  Form roughness and the absence of secondary flow in a large confluence–diffluence, Rio Paraná, Argentina , 2007 .

[20]  John J. Warwick,et al.  Full title page pp iii Modeling erosion and overbank deposition during extreme flood conditions on the Carson River, Nevada , 2004 .

[21]  Kandiah Arulanandan,et al.  Development of a quantitative method to predict critical shear stress and rate of erosion of natural undisturbed cohesive soils , 1980 .

[22]  Juha Hyyppä,et al.  Mapping Topography Changes and Elevation Accuracies Using a Mobile Laser Scanner , 2011, Remote. Sens..

[23]  P. Carling The geology of the lower Mekong river , 2009 .

[24]  D. Lague,et al.  Accurate 3D comparison of complex topography with terrestrial laser scanner: Application to the Rangitikei canyon (N-Z) , 2013, 1302.1183.

[25]  C. Renshaw,et al.  Impact of reach geometry on stream channel sensitivity to extreme floods , 2014 .

[26]  D. Raff,et al.  Assessing the ability of airborne LiDAR to map river bathymetry , 2008 .

[27]  Soo Chin Liew,et al.  The Mekong from satellite imagery: A quick look at a large river , 2007 .

[28]  W. Dietrich,et al.  A new framework for modeling the migration of meandering rivers , 2011 .

[29]  Michael M. Kazhdan,et al.  Poisson surface reconstruction , 2006, SGP '06.

[30]  Daniel R. Parsons,et al.  Velocity Mapping Toolbox (VMT): a processing and visualization suite for moving‐vessel ADCP measurements , 2011 .

[31]  J. Best,et al.  Morphology, flow structure, and suspended bed sediment transport at two large braid‐bar confluences , 2009 .

[32]  James E. Pizzuto,et al.  Quantifying bank erosion on the South River from 1937 to 2005, and its importance in assessing Hg contamination. , 2009 .

[33]  J. Best,et al.  Flow Structure and Transport of Sand‐Grade Suspended Sediment around an Evolving Braid Bar, Jamuna River, Bangladesh , 2009 .

[34]  Cheryl J. Hapke,et al.  National assessment of shoreline change part 4: historical coastal cliff retreat along the California coast , 2007 .

[35]  Damià Vericat,et al.  EVALUATING SHALLOW‐WATER BATHYMETRY FROM THROUGH‐WATER TERRESTRIAL LASER SCANNING UNDER A RANGE OF HYDRAULIC AND PHYSICAL WATER QUALITY CONDITIONS , 2014 .

[36]  J. Best,et al.  Extreme sediment pulses generated by bend cutoffs along a large meandering river , 2011 .

[37]  S. Lane,et al.  On the relationship between flow and suspended sediment transport over the crest of a sand dune, Río Paraná, Argentina , 2010 .

[38]  S. Schumm The Fluvial System , 1977 .

[39]  P. Atkinson,et al.  Decadal length changes in the fluvial planform of the River Ganga: bringing a mega-river to life with Landsat archives , 2013 .

[40]  J. W. Kean,et al.  Form drag in rivers due to small-scale natural topographic features : 2 . Irregular sequences , 2006 .

[41]  R. H. Meade,et al.  World-Wide Delivery of River Sediment to the Oceans , 1983, The Journal of Geology.

[42]  P. Y. Julien,et al.  Case Study: Bed Resistance of Rhine River during 1998 Flood , 2002 .

[43]  A. Schleiss,et al.  Influence of shallowness, bank inclination and bank roughness on the variability of flow patterns and boundary shear stress due to secondary currents in straight open-channels , 2010 .

[44]  J. Kean,et al.  Form drag in rivers due to small-scale natural topographic features: 2. Irregular sequences , 2006 .

[45]  J. Best,et al.  Morphological evolution and dynamics of a large, sand braid‐bar, Jamuna River, Bangladesh , 2000 .

[46]  Shaochuang Liu,et al.  Pinpointing source of Mekong and measuring its length through analysis of satellite imagery and field investigations , 2007 .

[47]  V. Baker Stream-channel response to floods, with examples from central Texas , 1977 .

[48]  M. Kummu,et al.  Fluvial sediment supply to a mega-delta reduced by shifting tropical-cyclone activity , 2016, Nature.

[49]  M. Kummu,et al.  Decoding the drivers of bank erosion on the Mekong river: The roles of the Asian monsoon, tropical storms, and snowmelt , 2013, Water resources research.

[50]  Greg . Smith,et al.  Can we distinguish flood frequency and magnitude in the sedimentological record of rivers , 2010 .

[51]  E. Latrubesse Patterns of anabranching channels: The ultimate end-member adjustment of mega rivers , 2008 .

[52]  Katherine L. Farnsworth,et al.  River Discharge to the Coastal Ocean: A Global Synthesis , 2011 .

[53]  J. Syvitski,et al.  Geomorphic/Tectonic Control of Sediment Discharge to the Ocean: The Importance of Small Mountainous Rivers , 1992, The Journal of Geology.

[54]  M. Allison,et al.  Bedform transport rates for the lowermost Mississippi River , 2008 .

[55]  L. James,et al.  Sediment characteristics of an extreme flood: 1993 upper Mississippi River valley , 1995 .

[56]  Bruno Merz,et al.  Flood trends and variability in the Mekong river , 2009 .

[57]  Xixi Lu,et al.  Riverbank changes along the Mekong River: Remote sensing detection in the Vientiane–Nong Khai area , 2008 .

[58]  Juha Hyyppä,et al.  Seamless Mapping of River Channels at High Resolution Using Mobile LiDAR and UAV-Photography , 2013, Remote. Sens..

[59]  Zhengyi Yao,et al.  Bank erosion and accretion along the Ningxia–Inner Mongolia reaches of the Yellow River from 1958 to 2008 , 2011 .

[60]  Juha Hyyppä,et al.  Data Processing and Quality Evaluation of a Boat-Based Mobile Laser Scanning System , 2013, Sensors.

[61]  J. Brasington,et al.  Hyperscale terrain modelling of braided rivers: fusing mobile terrestrial laser scanning and optical bathymetric mapping , 2014 .

[62]  S. Lane,et al.  Morphology and flow fields of three‐dimensional dunes, Rio Paraná, Argentina: Results from simultaneous multibeam echo sounding and acoustic Doppler current profiling , 2005 .

[63]  M. Guerrero,et al.  Flow Field and Morphology Mapping Using ADCP and Multibeam Techniques: Survey in the Po River , 2011 .

[64]  Les Basher,et al.  Measurement of river bank and cliff erosion from sequential LIDAR and historical aerial photography , 2011 .

[65]  J. Best,et al.  Measuring flow velocity and sediment transport with an acoustic Doppler current profiler , 2005 .

[66]  A. Miller Flood hydrology and geomorphic effectiveness in the central Appalachians , 1990 .

[67]  V. Kale,et al.  Effectiveness of monsoon floods on the Tapi River, India: role of channel geometry and hydrologic regime , 2004 .

[68]  E. Robert Thieler,et al.  The Digital Shoreline Analysis System (DSAS) Version 4.0 - An ArcGIS extension for calculating shoreline change , 2009 .

[69]  M. O'Neal,et al.  The rates and spatial patterns of annual riverbank erosion revealed through terrestrial laser‐scanner surveys of the South River, Virginia , 2011 .

[70]  Emmanuel Partheniades,et al.  Erosion and Deposition of Cohesive Soils , 1965 .

[71]  Julian Leyland,et al.  A self‐limiting bank erosion mechanism? inferring temporal variations in bank form and skin drag from high resolution topographic data , 2015 .

[72]  Avijit Gupta High‐Magnitude Floods and Stream Channel Response , 2009 .

[73]  Matti Kummu,et al.  Spatio-temporal scales of hydrological impact assessment in large river basins: the Mekong case , 2008 .

[74]  G. Heritage,et al.  Towards a protocol for laser scanning in fluvial geomorphology , 2007 .

[75]  Qiuwen Chen,et al.  Flow processes near smooth and rough (concave) outer banks in curved open channels , 2012 .

[76]  Murray C. Peel,et al.  The Hydrology of the Mekong River , 2009 .

[77]  I. Overeem,et al.  Sinking deltas due to human activities , 2009 .