Exploring the contributions of vegetation and dune size to early dune development using unmanned aerial vehicle (UAV) imaging

Abstract. Dune development along highly dynamic land–sea boundaries is the result of interaction between vegetation and dune size with sedimentation and erosion processes. Disentangling the contribution of vegetation characteristics from that of dune size would improve predictions of nebkha dune development under a changing climate, but has proven difficult due to the scarcity of spatially continuous monitoring data. This study explored the contributions of vegetation and dune size to dune development for locations differing in shelter from the sea. We monitored a natural nebkha dune field of 8 ha, along the coast of the island Texel, the Netherlands, for 1 year using an unmanned aerial vehicle (UAV) with camera. After constructing a digital surface model and orthomosaic we derived for each dune (1) vegetation characteristics (species composition, vegetation density, and maximum vegetation height), (2) dune size (dune volume, area, and maximum height), (3) degree of shelter (proximity to other nebkha dunes and the sheltering by the foredune). Changes in dune volume over summer and winter were related to vegetation, dune size and degree of shelter. We found that a positive change in dune volume (dune growth) was linearly related to initial dune volume over summer but not over winter. Big dunes accumulated more sand than small dunes due to their larger surface area. Exposed dunes increased more in volume (0.81 % per dune per week) than sheltered dunes (0.2 % per dune per week) over summer, while the opposite occurred over winter. Vegetation characteristics did not significantly affect dune growth in summer, but did significantly affect dune growth in winter. Over winter, dunes dominated by Ammophila arenaria, a grass species with high vegetation density throughout the year, increased more in volume than dunes dominated by Elytrigia juncea, a grass species with lower vegetation density (0.43 vs. 0.42 (m3 m−3) week−1). The effect of species was irrespective of dune size or distance to the sea. Our results show that dune growth in summer is mainly determined by dune size, whereas in winter dune growth was determined by vegetation type. In our study area the growth of exposed dunes was likely restricted by storm erosion, whereas growth of sheltered dunes was restricted by sand supply. Our results can be used to improve models predicting coastal dune development.

[1]  R. Feagin,et al.  Response of vegetated dune–beach systems to storm conditions , 2016 .

[2]  R. Carter Near-future sea level impacts on coastal dune landscapes , 1991, Landscape Ecology.

[3]  Z. Dong,et al.  The blown sand flux over a sandy surface: a wind tunnel investigation on the fetch effect , 2004 .

[4]  Samantha E. Saye,et al.  Beach–dune morphological relationships and erosion/accretion: An investigation at five sites in England and Wales using LIDAR data , 2005 .

[5]  Jennifer M. Brown,et al.  Comparison of storm cluster vs isolated event impacts on beach/dune morphodynamics , 2015 .

[6]  T. Hothorn,et al.  Simultaneous Inference in General Parametric Models , 2008, Biometrical journal. Biometrische Zeitschrift.

[7]  J. A. Hartigan,et al.  A k-means clustering algorithm , 1979 .

[8]  Sanford Weisberg,et al.  An R Companion to Applied Regression , 2010 .

[9]  I. Delgado‐Fernandez A review of the application of the fetch effect to modelling sand supply to coastal foredunes , 2010 .

[10]  H. Nepf,et al.  Flow patterns around two neighboring patches of emergent vegetation and possible implications for deposition and vegetation growth , 2015, Environmental Fluid Mechanics.

[11]  R. Crawford The biology of coastal sand dunes , 2009 .

[12]  Peter Ruggiero,et al.  Biophysical feedback mediates effects of invasive grasses on coastal dune shape. , 2012, Ecology.

[13]  Orencio Durán,et al.  Vegetation controls on the maximum size of coastal dunes , 2013, Proceedings of the National Academy of Sciences.

[14]  Óscar Ferreira,et al.  The role of storm groups in the erosion of sandy coasts , 2006 .

[15]  Carrie V. Kappel,et al.  Non‐linearity in ecosystem services: temporal and spatial variability in coastal protection , 2009 .

[16]  M. Westoby,et al.  ‘Structure-from-Motion’ photogrammetry: A low-cost, effective tool for geoscience applications , 2012 .

[17]  J. Al-awadhi,et al.  Morphological characteristics and development of coastal nabkhas, north-east Kuwait , 2013, International Journal of Earth Sciences.

[18]  M. Martínez,et al.  Coastal dunes: ecology and conservation. , 2004 .

[19]  J. Keijsers,et al.  Vegetation and sedimentation on coastal foredunes , 2015 .

[20]  Xiaofeng Wang,et al.  Wind tunnel experiments of air flow patterns over nabkhas modeled after those from the Hotan River basin, Xinjiang, China (I): non-vegetated , 2008 .

[21]  S. M. Arens Patterns of sand transport on vegetated foredunes , 1996 .

[22]  J. Keijsers,et al.  Modeling the biogeomorphic evolution of coastal dunes in response to climate change , 2016 .

[23]  A. Gunatilaka,et al.  Flow separation and the internal structure of shadow dunes , 1989 .

[24]  Peter Ruggiero,et al.  Invasive grasses, climate change, and exposure to storm‐wave overtopping in coastal dune ecosystems , 2013, Global change biology.

[25]  J. Bakker Phytogeographical aspects of the vegetation of the outer dunes in the Atlantic province of Europe , 1976 .

[26]  Robert A. Holman,et al.  Wave run-up on a high-energy dissipative beach , 2004 .

[27]  E. Anthony Storms, shoreface morphodynamics, sand supply, and the accretion and erosion of coastal dune barriers in the southern North Sea , 2013 .

[28]  Pier Vellinga,et al.  Beach and dune erosion during storm surges , 1982 .

[29]  J. MacQueen Some methods for classification and analysis of multivariate observations , 1967 .

[30]  H. N. Southgate,et al.  Dune behavior and aeolian transport on decadal timescales , 2012 .

[31]  Z. Dong,et al.  Near-wake flow patterns in the lee of adjacent obstacles and their implications for the formation of sand drifts: A wind tunnel simulation of the effects of gap spacing , 2014 .

[32]  P. Slim,et al.  Embryo dune development drivers: beach morphology, growing season precipitation, and storms , 2017 .

[33]  Mark A. Fonstad,et al.  Topographic structure from motion: a new development in photogrammetric measurement , 2013 .

[34]  A. Poortinga,et al.  Spatio-Temporal Variability in Accretion and Erosion of Coastal Foredunes in the Netherlands: Regional Climate and Local Topography , 2014, PloS one.

[35]  Juha Suomalainen,et al.  A Lightweight Hyperspectral Mapping System and Photogrammetric Processing Chain for Unmanned Aerial Vehicles , 2014, Remote. Sens..

[36]  J. Langley,et al.  A species effect on storm erosion: Invasive sedge stabilized dunes more than native grass during Hurricane Sandy , 2017 .

[37]  B. Hallet Spatial self-organization in geomorphology: from periodic bedforms and patterned ground to scale-invariant topography , 1990 .

[38]  Bill Watts,et al.  Have we neglected the societal importance of sand dunes? An ecosystem services perspective , 2010 .

[39]  P. Hesp Foredunes and blowouts: initiation, geomorphology and dynamics , 2002 .

[40]  P. Hesp,et al.  Nebkha flow dynamics and shadow dune formation , 2017 .

[41]  C. Houser,et al.  Controls on coastal dune morphology, shoreline erosion and barrier island response to extreme storms , 2008 .

[42]  Yaping Shao,et al.  The overshoot and equilibration of saltation , 1992 .

[43]  P. Hesp Morphology, dynamics and internal stratification of some established foredunes in southeast Australia , 1988 .

[44]  Ping Wang,et al.  Factors controlling the survival of coastal dunes during multiple hurricane impacts in 2004 and 2005: Santa Rosa barrier island, Florida , 2008 .

[45]  P. Yan,et al.  The progress and prospects of nebkhas in arid areas , 2010 .

[46]  R. Houthuys,et al.  Definition of storm thresholds for significant morphological change of the sandy beaches along the Belgian coastline , 2012 .

[47]  P. Lu,et al.  Wind tunnel simulation of the three‐dimensional airflow patterns around shrubs , 2008 .

[48]  P. Zarnetske,et al.  Subtle differences in two non-native congeneric beach grasses significantly affect their colonization, spread, and impact , 2012 .

[49]  Patrick A. Hesp,et al.  The formation of shadow dunes , 1981 .

[50]  Douglas J. Sherman,et al.  Coastal erosion, global sea-level rise, and the loss of sand dune plant habitats , 2005 .

[51]  Ian J. Walker,et al.  Dynamics of secondary airflow and sediment transport over and in the lee of transverse dunes , 2002 .

[52]  Peter M. J. Herman,et al.  Spatial flow and sedimentation patterns within patches of epibenthic structures: Combining field, flume and modelling experiments , 2007 .

[53]  A. Baas Chaos, fractals and self-organization in coastal geomorphology: simulating dune landscapes in vegetated environments , 2002 .

[54]  T. Carlson,et al.  On the relation between NDVI, fractional vegetation cover, and leaf area index , 1997 .

[55]  Jim H. Chandler,et al.  Decadal and seasonal development of embryo dunes on an accreting macrotidal beach: North Lincolnshire, UK , 2013 .