-
Impact of climate on landscape form, sediment transfer, and the sedimentary record Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-18 Rebekah M. Harries; Boris Gailleton; Linda A. Kirstein; Mikael Attal; Alexander C. Whittaker; Simon M. Mudd
The relationship between climate, landscape connectivity and sediment export from mountain ranges is key to understanding the propagation of erosion signals downstream into sedimentary basins. We explore the role of connectivity in modulating the composition of sediment exported from the Frontal Cordillera of the south central Argentine Andes by comparing three adjacent and apparently similar semi‐glaciated
-
Assessment of magnetite as a magnetic tracer for sediments in the study of ephemeral gully erosion: conditioning factors of magnetic susceptibility Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-17 Elena Zubieta; Juan C. Larrasoaña; Alaitz Aldaz; Javier Casalí; Rafael Giménez
In gully erosion, the detached soil can be transported over long distances along the landscape. The eroded material can be redistributed and/or deposited on the soil surface along the landscape and then eventually be buried by newly eroded and deposited sediment. There can be significant variability of the soil conditions (e.g., texture and moisture content) over which the eroded material travels.
-
Observations on decadal sandbar behaviour along a large‐scale curved shoreline Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-28 R. Gijsman; B.G. Ruessink; J. Visscher; T. Schlurmann
-
Hillslope erosion in a grassland environment: Calibration and evaluation of the SIBERIA landscape evolution model Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-28 G.R. Hancock; Abraham Gibson; T. Wells
-
Where will widening occur in an outwash braidplain? A new approach to detecting controls on fluvial lateral erosion in a glacierized catchment (NW Spitsbergen, Svalbard) Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-15 Piotr Weckwerth; Ireneusz Sobota; Katarzyna Greń
The dynamics of fluvial system evolution depend on fluvial processes and their driving forces associated with climatic variations, which affect changes in the morphology of river channels and floodplains. Neither channel slope and morphology, nor the properties of fluvial sediment have previously been considered as determinants of active braidplain widening on outwash plains (formed from valley/alpine
-
Signal crayfish burrowing, bank retreat and sediment supply to rivers: a biophysical sediment budget Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-15 H. Sanders; S.P. Rice; P.J. Wood
Burrowing into riverbanks by animals transfers sediment directly into river channels and has been hypothesised to accelerate bank erosion and promote mass failure. A field monitoring study on two UK rivers invaded by signal crayfish (Pacifastacus leniusculus) assessed the impact of burrowing on bank erosion processes. Erosion pins were installed in 17 riverbanks across a gradient of crayfish burrow
-
Video monitoring of in‐channel wood: from flux characterization and prediction to recommendations to equip stations Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-15 Zhang Zhi; Hossein Ghaffarian; Bruce MacVicar; Lise Vaudor; Aurélie Antonio; Kristell Michel; Hervé Piégay
Wood flux (piece number per time interval) is a key parameter for understanding wood budgeting, determining the controlling factors, and managing flood risk in a river basin. Quantitative wood flux data is critically needed to improve the understanding of wood dynamics and estimate wood discharge in rivers. In this study, the streamside videography technique was applied to detect wood passage and measure
-
Late‐Quaternary Miliolite (biogenic carbonate) deposits and their implications for sea‐level fluctuations and climatic variability Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-15 A. Durga Prasad; Falguni Bhattacharya; Gaurav Chauhan; D. Balaji; M.G. Thakkar; Y. Srinivasa Rao
The western coast of India (Kachchh) has ubiquitous preservations of Quaternary carbonate deposits popularly known as “Miliolites”. Field‐based detail documentation of the nature and distribution of miliolites supported by sedimentology and SEM microtextural studies indicates that the miliolites were primarily deposited by wind as aeolinites and are termed “Primary Miliolites (PM)”. These were subsequently
-
Mechanisms for avulsion on alluvial fans: insights from high‐frequency topographic data Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-14 Anya Leenman; Brett Eaton
Avulsion is a key process in building alluvial fans, but it is also a formidable natural hazard. Based on laboratory experiments monitored with novel high‐frequency photogrammetry, we present a new model for avulsion on widely graded gravel fans. Previous experimental studies of alluvial fans have suggested that avulsion occurs in a periodic autogenic cycle, that is thought to be mediated by the gradient
-
Zircon provenance of Quaternary cover beds using U‐Pb dating: regional differences in the south‐western USA Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-14 Jana Richter‐Krautz; Mandy Hofmann; Johannes Zieger; Ulf Linnemann; Arno Kleber
U‐Pb dating of detrital zircons (DZ) in Quaternary slope deposits (cover beds) and the examination of the surface structure of single zircon grains may allow reconstructing the provenance of their aeolian components and may help to reconstruct sedimentary palaeo‐transportation cascades. We distinguish several layers of slope deposits (cover beds), using a palaeosol‐supported sequence‐stratigraphic
-
Experimental investigation of the morphodynamic response of riffles and pools to unsteady flow and increased sediment supply Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-12 Jacob A. Morgan; Peter A. Nelson
Gravel‐bed rivers characteristically exhibit shallow riffles in wide sections and deeper pools where the channel becomes constricted and narrow. While rivers can adjust to changing flow and sediment supply through some combination of adjustments of channel slope, bed‐surface sorting, and channel shape, the degree to which riffle‐pools may adopt these changes in response to changing flows and sediment
-
Generation of realistic synthetic catchments to explore fine continental surface processes Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-14 Raphaël Bunel; Nicolas Lecoq; Yoann Copard; Eric Guérin; Marco Van de Wiel; Nicolas Massei
-
Late Holocene flood magnitudes in the Lower Rhine river valley and upper delta resolved by a two‐dimensional hydraulic modelling approach Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-11 Bas van der Meulen; Anouk Bomers; Kim M. Cohen; Hans Middelkoop
Palaeoflood hydraulic modelling is essential for quantifying ‘millennial flood’ events not covered in the instrumental record. Palaeoflood modelling research has largely focused on one‐dimensional analysis for geomorphologically stable fluvial settings, because two‐dimensional analysis for dynamic alluvial settings is time‐consuming and requires a detailed representation of the past landscape. In this
-
A morphological investigation of marine transgression in estuaries Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-25 Ian Townend; Zeng Zhou; Leicheng Guo; Giovanni Coco
-
A method for estimating sediment budgets of washover deposits using Digital Terrain Models Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-06 Lars Ø. Hansen; Verner B. Ernstsen; Lars B. Clemmensen; Zyad Al‐Hamdani; Aart Kroon
Washover fans are located on small barriers in fetch‐limited micro‐tidal coastal environments in Denmark. These washover fans are formed during high‐energy storm events and we present a method to quantify their volumes and to estimate sediment exchanges between washover fans and their adjacent morphologies. We use high resolution Digital Terrain Models (DTMs) based on LiDAR data. We have delineated
-
Gully prevention and control: Techniques, failures and effectiveness Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-09 Amaury Frankl; Jan Nyssen; Matthias Vanmaercke; Jean Poesen
-
Evolution of debris cover on glaciers of the Eastern Alps, Austria, between 1996 and 2015 Earth Surf.Process. Land. (IF 3.694) Pub Date : 2021-01-02 Fabian Fleischer; Jan‐Christoph Otto; Robert R. Junker; Daniel Hölbling
Debris cover on glaciers is an important component of glacial systems as it influences climate‐glacier dynamics and thus the lifespan of glaciers. Increasing air temperatures, permafrost thaw, as well as rock faces freshly exposed by glacier downwasting in accumulation zones result in increased rockfall activity and debris input. In the ablation zone, negative mass balances result in an enhanced melt‐out
-
Surface velocity fields of active rock glaciers and ice‐debris complexes in the Central Andes of Argentina Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-02 Jan Henrik Blöthe; Christian Halla; Ellen Schwalbe; Estefania Bottegal; Dario Trombotto Liaudat; Lothar Schrott
-
Formation of asymmetrical loess gullies in the northeastern Loess Plateau of China Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-29 Si‐Ming Chen; Li‐Yang Xiong; Jia‐Zhen Duan; Guo‐An Tang
Loess gullies are the most active and changeable landform unit on the Loess Plateau of China. Under the influence of inhomogeneous internal and external forces, various gully morphologies have been identified as specific forms of asymmetrical loess gullies in the northeastern Loess Plateau. Thus, the formation mechanisms of asymmetrical gullies should be examined to better understand the gully evolution
-
Rill and ephemeral gully erosion in a small olive grove catchment in Spain: interactions between management and conservation measures Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-29 E.V. Taguas
Concentrated flow erosion in Mediterranean cultivated areas is considered a major process of land degradation. Rills and ephemeral gullies in a 6.4 ha olive orchard catchment located in an intensive commercial farm which could represent a common degradation scenario in hilly areas, were measured and compared with the sediment loads at the outlet. 4 GPS survey campaigns were done between March‐2009
-
Analysis of rill step‐pool morphology and its comparison with stream case Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-29 V. Pampalone; C. Di Stefano; A. Nicosia; V. Palmeri; V. Ferro
In this paper the morphology of step‐pool features is analyzed using rill measurements and literature data for streams. Close‐range photogrammetry was used to carry out ground measurements on rills with step‐pool units, shaped on a plot having slope equal to 14%, 15%, 22%, 24%, and 26%. Data were used to compare the relationships between H/L, in which H is the step height and L is the step length,
-
Landslide Susceptibility Analysis Based on Citizen Reports Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-29 Tyler J. Rohan; Nicholas Wondolowski; Eitan Shelef
Landslide susceptibility estimates are essential for reducing the risk posed by landslides to social and economic well‐being. However, estimates of landslide susceptibility depend on reliable landslide inventories whose production requires extensive field or remote sensing efforts. Further, most inventories are not updated through time and thus may not capture the influence of changes in climate and/or
-
Geometry of obstacle marks at instream boulders – integration of laboratory investigations and field observations Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-23 Oliver Schlömer; Paul E. Grams; Daniel Buscombe; Jürgen Herget
Obstacle marks are instream bedforms, typically composed of an upstream frontal scour hole and a downstream sediment accumulation in the vicinity of an obstacle. Local scouring at infrastructure (e.g. bridge piers) is a well‐studied phenomenon in hydraulic engineering, while less attention is given to the time‐dependent evolution of frontal scour holes at instream boulders and their geometrical relations
-
Past, present and future of a meandering river in the Bolivian Amazon basin Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-22 Kattia Rubi Arnez Ferrel; Jonathan Mark Nelson; Yasuyuki Shimizu; Tomoko Kyuka
Field observations on small rivers of the Amazon basin are less common due to their remote location and difficult accessibility. Here, we show through remote sensing analysis and field works, the planform evolution and riverbed topography of a small river located in the upper foreland Amazon basin, the Ichilo river. By tracking planform changes along 30 years we identified the factors that control
-
Logjams as a Driver of Transient Storage in a Mountain Stream Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-22 Ethan Ader; Ellen Wohl; Sawyer McFadden; Kamini Singha
We use four stream segments along a wood‐rich, pool‐riffle mountain stream in the Southern Rockies of Colorado, USA to examine how spatial variations in wood load and variations in discharge during and after the snowmelt peak flow influence the magnitude of surface and subsurface transient storage. Segments range in complexity from a single channel with no large wood to an anabranching channel with
-
Modelling future lahars controlled by different volcanic eruption scenarios at Cotopaxi (Ecuador) calibrated with the massively destructive 1877 lahar Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-22 Theresa Frimberger; Daniel Andrade; Samuel Weber; Michael Krautblatter
Lahars are among the most hazardous mass flow processes on earth and have caused up to 23,000 casualties in single events in the recent past. The Cotopaxi volcano, 60 km southeast of Quito, has a well‐documented history of massively destructive lahars and is a hotspot for future lahars due to (i) its ~10 km2 glacier cap, (ii) its 117‐147‐year return period of (Sub)‐Plinian eruptions and (iii) the densely
-
Wildfire and Earth Surface Processes Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-17 F.K. Rengers; Luke A. McGuire
Wildfire is a landscape‐scale disturbance that changes the rate and magnitude of many earth surface processes. The impacts of fire on earth surface processes can vary substantially from place to place depending on a variety of site‐specific conditions, including topography, fire severity, regional climate, vegetation type, and soil type. This variation makes it critical to bring together scientists
-
Estimation of discharges of water flows and debris floods in a small watershed Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-17 Xiaojun Guo; Peng Cui; Xingchang Chen; Yong Li; Ju Zhang; Yuqing Sun
Floods in small mountainous watersheds cover a wide spectrum of flow. They can range from clear water flows and hyperconcentrated flows to debris floods and debris flows, and calculation of the peak discharge is crucial for predicting and mitigating such hazards. To determine the optimal approach for discharge estimation, this study compared water flow monitoring hydrographs to investigate the performance
-
The spatial distribution of sedimentary compounds and their environmental implications in surface sediments of Lake Khar Nuur (Mongolian Altai) Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-14 P. Strobel; J. Struck; R. Zech; M. Bliedtner
Lake sediments are valuable natural archives to reconstruct paleoclimate and ‐environmental changes which consist of inorganic and organic sediment compounds of allochthonous origin from the catchment and of autochthonous production in the lake. However, for robust paleo‐reconstructions it is important to develop a better understanding about sedimentation processes, the origin of inorganic and organic
-
Morphodynamic effects of vegetation life stage on experimental meandering channels Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-14 Tomoko Kyuka; Satomi Yamaguchi; Yusuke Inoue; Kattia Rubi Arnez Ferrel; Hideto Kon; Yasuyuki Shimizu
Previous studies have demonstrated that riparian vegetation leads to channel transformation from a multi‐bar to a single‐thread channel planform. However, it still remains unclear how the presence of pioneer and mature vegetation affects the morphodynamics of single‐thread meandering rivers. In this study, we therefore investigated the effects of vegetation strength on the morphodynamic evolution of
-
Relating Millimeter‐scale Turbulence to Meter‐scale Subtidal Erosion and Accretion across the Fringe of a Coastal Mangrove Forest Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-14 Benjamin K. Norris; Julia C. Mullarney; Karin R. Bryan; Stephen M. Henderson
Within a wave‐exposed mangrove forest, novel field observations are presented, comparing millimeter‐scale turbulent water velocity fluctuations with contemporaneous subtidal bed elevation changes. High‐resolution velocity and bed level measurements were collected from the unvegetated mudflat, at the mangrove forest fringe, and within the forest interior over multiple tidal cycles (flood‐ebb) during
-
A modified Raupach's Model applicable for shear‐stress partitioning on surfaces covered with dense and flat‐shaped gravel roughness elements Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-14 Huiru Li; Xueyong Zou; Mengcui Zhang; Liqiang Kang; Chunlai Zhang; Hong Cheng; Xiaoxu Wu
A commonly‐used measure to prevent soil wind erosion is to cover the surface with gravel. Gravel can inhibit soil erosion by covering the surface directly, changing the airflow field near the surface, and sharing the shear stress of wind. Similar to other roughness elements, the protective effect of gravel on soil is usually expressed in terms of the ratio of the shear stress on the exposed soil surface
-
Issue Information Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-13
No abstract is available for this article. © 2020 John Wiley & Sons, Ltd.
-
Modeling the effect of saltation on surface layer turbulence Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-06 Hao‐Jie Huang
-
Evaluating debris‐flow and anthropogenic disturbance on 10Be concentration in mountain drainage basins: implications for functional connectivity and denudation rates across time scales Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-06 Francesco Brardinoni; Reto Grischott; Florian Kober; Corrado Morelli; Marcus Christl
-
What is wrong with post‐fire soil erosion modelling? A meta‐analysis on current approaches, research gaps, and future directions Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-12 A.R. Lopes; A. Girona‐García; S. Corticeiro; R. Martins; J.J. Keizer; D.C.S. Vieira
-
Comparing Single‐Phase, Non‐Newtonian Approaches to Experimental Results: Validating Flume‐Scale Mud and Debris Flow in HEC‐RAS Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-10 S. Gibson; I. Floyd; A. Sánchez; R. Heath
Post‐fire debris flows and tailing impoundment failures destroy lives and property. These geologic hazards—and other similar processes—fall on a continuum between classic Newtonian flood analyses and geotechnical stability analyses. The US Army Corps of Engineers (USACE) is developing a Non‐Newtonian library (DebrisLib) that includes a suite of rheological and clastic approaches to hyper‐concentrated
-
Modelling of sediment supply from torrent catchments in the Western Alps using the Sediment Contributing Area (SCA) approach Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-08 Moritz Altmann; Florian Haas; Tobias Heckmann; Frédéric Liébault; Michael Becht
The production of coarse sediment in mountain landscapes results mainly from the type and activity of geomorphic processes and topographic and natural conditions (e.g. vegetation cover) of these catchments. The supply of sediment from these slopes to mountain streams and the subsequent transport lead to sediment connectivity, that describes the integrated coupling state of these systems. Studies from
-
Rapid Tidal Marsh Development in Anthropogenic Backwaters Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-08 Brian Yellen; Jonathan Woodruff; Caroline Ladlow; David K. Ralston; Sarah Fernald; Waverly Lau
Tidal marsh restoration and creation is growing in popularity due to the many and diverse set of services these important ecosystems provide. However, it is unclear what conditions within constructed settings will lead to the successful establishment of tidal marsh. Here we provide documentation for widespread and rapid development of tidal freshwater wetlands for a major urban estuary as an unintended
-
Sediment cascades and the entangled relationship between human impact and natural dynamics at the pre‐pottery Neolithic site of Göbekli Tepe, Anatolia Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-16 Moritz Nykamp; Fabian Becker; Ricarda Braun; Nadja Pöllath; Daniel Knitter; Joris Peters; Brigitta Schütt
-
Morphology and evolution of supraglacial hummocks on debris‐covered Himalayan glaciers Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-12-03 Oliver T. Bartlett; Felix S.L. Ng; Ann V. Rowan
Thick supraglacial debris layers often have an undulating, hummocky topography that influences the lateral transport of debris and meltwater and provides basins for supraglacial ponds. The role of ablation and other processes associated with supraglacial debris in giving rise to this hummocky topography is poorly understood. Characterising hummocky topography is a first step towards understanding the
-
Quantification of permafrost creep provides kinematic evidence for classifying a puzzling periglacial landform Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-23 Yan Hu; Lin Liu; Xiaowen Wang; Lin Zhao; Tonghua Wu; Jialun Cai; Xiaofan Zhu; Junming Hao
-
Hillslope sediment fence catch efficiencies and particle sorting for post‐fire rain storms Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-21 Codie Wilson; Stephanie K. Kampf; Joseph W. Wagenbrenner; Lee H. MacDonald; Hunter Gleason
-
Robust methods for the decomposition and interpretation of compound dunes applied to a complex hydro‐morphological setting Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-28 Leon Scheiber; Oliver Lojek; Axel Götschenberg; Jan Visscher; Torsten Schlurmann
Underwater dunes are a morphological feature that are explored by marine scientists and coastal engineers alike. This study presents new methodologies in order to simplify bedform identification and morphodynamic analyses. Specifically, subaqueous compound dunes are decomposed with a simple yet extensive tracking algorithm which relies on a repeated evaluation of unfiltered bed elevation profiles according
-
The behaviour of beach elevation contours in response to different wave energy environments Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-16 Wenhong Pang; Zhenpeng Ge; Zhijun Dai; Shushi Li; Hu Huang
-
Controls of alluvial cover formation, morphology and bedload transport in a sinuous channel with a non‐alluvial boundary Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-03 E. Papangelakis; M. Welber; P. Ashmore; B. MacVicar
-
Seismic constraints on rock damaging related to a failing mountain peak: the Hochvogel, Allgäu Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-16 M. Dietze; M. Krautblatter; L. Illien; N. Hovius
-
Planform‐asymmetry and backwater effects on river‐cutoff kinematics and clustering Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-30 Alessandro Ielpi; Mathieu G.A. Lapôtre; Alvise Finotello; Massimiliano Ghinassi
-
Supergene sulphuric acid speleogenesis and the origin of hypogene caves: evidence from the Northern Pennines, UK Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-17 John A. Webb
-
High‐resolution fjord sediment record of a receding glacier with growing intermediate proglacial lake (Steffen Fjord, Chilean Patagonia) Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-10 Loic Piret; Sebastien Bertrand; Jon Hawkings; Malin E. Kylander; Fernando Torrejón; Benjamin Amann; Jemma Wadham
-
Equality, diversity, inclusion: ensuring a resilient future for geomorphology Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-20 Stephen Tooth; Heather A. Viles
Within and beyond academia, debates around equality, diversity and inclusion (EDI) have been gathering pace. We focus on EDI and geomorphology and address four main questions: (1) why does EDI matter for geomorphology?; (2) what are the barriers to greater EDI in geomorphology?; (3) how can we address these EDI barriers?; (4) can we ensure a resilient future for geomorphology by addressing EDI? At
-
Biogeomorphology, quo vadis? On processes, time, and space in biogeomorphology Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-10 A. Larsen; W. Nardin; W.I. van de Lageweg; N. Bätz
-
Large wood load fluctuations in an Andean basin Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-11-03 Lorenzo Picco; Cordelia Scalari; Andrés Iroumé; Bruno Mazzorana; Andrea Andreoli
-
Analysis of historical data for a better understanding of post‐construction landslides at an artificial waterway Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-29 Annika Wohlers; Bodo Damm
-
The active layer in gravel‐bed rivers: An empirical appraisal Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-22 D. Vázquez‐Tarrío; G. Piqué; D. Vericat; R.J. Batalla
-
Field measurements of shear stress and friction in the surf zone Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-30 Troels Aagaard; Drude F. Christensen; Michael G. Hughes
-
Evaluating young fluvial terrace riser degradation using a nonlinear transport model: Application to the Kongur Normal Fault in the Pamir, northwest China Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-16 Jianhong Xu; J Ramón Arrowsmith; Jie Chen; Lindsay M. Schoenbohm; Tao Li; Zhaode Yuan; Lewis A. Owen
-
Seven decades of hydrogeomorphological changes in a near‐natural (Sense River) and a hydropower‐regulated (Sarine River) pre‐Alpine river floodplain in Western Switzerland Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-10 Diego Tonolla; Martin Geilhausen; Michael Doering
-
Impact of an 0.2 km3 Rock Avalanche on Lake Eibsee (Bavarian Alps, Germany) – Part I: Reconstruction of the paleolake and Effects of the Impact Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-17 Sibylle Knapp; Philipp Mamot; Bernhard Lempe; Michael Krautblatter
-
Impact of an 0.2 km3 Rock Avalanche on Lake Eibsee (Bavarian Alps, Germany) – Part II: Catchment Response to Consecutive Debris Avalanche and Debris Flow Earth Surf.Process. Land. (IF 3.694) Pub Date : 2020-10-17 Sibylle Knapp; Flavio S. Anselmetti; Bernhard Lempe; Michael Krautblatter
Contents have been reproduced by permission of the publishers.