Abstract

While remote sensing methods have long been used for coastal and desert sand dune studies, few methods have been developed for the automated measurement of dune migration in large dune fields. To overcome a major limitation of an existing method named “pairs of source and target points (PSTP)”, this paper proposes a toe line tracking (TLT) method for the automated measurement of dune migration rate and direction using multi-temporal digital elevation models (DEM) derived from light detection and ranging (LiDAR) data. Based on a few simple parameters, the TLT method automatically extracts the base level of a dune field and toe lines of individual dunes. The toe line polygons derived from two DEMs are processed using logical operators and other spatial analysis methods implemented in the Python programming language in a geographic information system. By generating thousands of random sampling points along source toe lines, dune migration distances and directions are calculated and saved with the sampling point feature class. The application of the TLT method was demonstrated using multi-temporal LiDAR-derived DEMs for a 9 km by 2.4 km area in the White Sands Dune Field in New Mexico (USA). Dune migration distances and directions for three periods (24 January 2009–26 September 2009, 26 September 2009–6 June 2010, and 24 January 2009–6 January 2010) were calculated. Sensitivity analyses were carried out using different window sizes and toe heights. The results suggest that both PSTP and TLT produce similar sand dune migration rates and directions, but TLT is a more generic method that works for dunes with or without slipfaces that reach the angle of repose.

Highlights

  • Understanding how sand dunes form and change on Earth and some other planets has long been a research topic in Earth and planetary surface processes [1,2,3,4,5,6,7,8]

  • After reviewing the limitation of the existing pairs ofinformation source and target points (PSTP) method for measuring sand dune migration rate and migration direction, this paper introduced a toe line tracking (TLT)

  • Method and implemented the new method using the Python programming language for automated measurement of dune migration distance and direction based on multi-temporal

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Summary

Introduction

Understanding how sand dunes form and change on Earth and some other planets (such as Mars, Venus, and Titan) has long been a research topic in Earth and planetary surface processes [1,2,3,4,5,6,7,8]. While studies in the 1970s and 1980s mainly focused on individual sand dunes, the advances in data collection and analysis enable studying dunes as complex systems [9], including numerous field studies around the world [10,11,12,13,14,15], quantitative/numerical models [16,17,18,19,20,21], and remote sensing methods [22,23,24,25,26,27,28,29,30,31,32,33,34,35] These studies have led to a better understanding of sand dunes.

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