Abstract

Glacial landforms are a significant element of landscape in many regions of Earth. The increasing availability of high-resolution digital elevation models (DEMs) provides an opportunity to develop automated methods of glacial landscape exploration and classification. In this study, we aimed to: 1) identify glacial landforms based on high-resolution DEM datasets; 2) determine relevant geomorphometric and spectral parameters and object-based features for the mapping of glacial landforms; and 3) develop an accurate workflow for glacial landform classification based on DEM. The developed methodology included the extraction of secondary features from DEM, feature selection with the Boruta algorithm, object-based image analysis, and random forest supervised classification. We applied the workflow for three study sites: one in Svalbard and two in Poland. It allowed the identification of six categories of glacial landforms: till plains, end moraines, hummocky moraines, outwash/glaciolacustrine plains, valleys, and kettle holes. The majority of relevant secondary features represented DEM spectral parameters calculated from 2-D Fourier analysis. The supervised classification models with the highest performance exhibited up to 96% overall accuracy with regard to a groundtruth dataset. This study showed that glacial landforms can be identified using novel image-processing methodology and spectral parameters of high-resolution DEM. The complete classification workflow developed herein provides a solution for the transparent generation of thematic maps of glacial landforms that may be reproducible and transferrable to various glacial regions worldwide.

Highlights

  • G EOMORPHOLOGY is an interdisciplinary field studying the distribution, size, morphology, and age of landforms, as well as processes shaping the Earth’s surface

  • Conspicuous glacial landforms located on the foreland of Elise glacier were formed as a result of glacier retreat from its maximum Little Ice Age (LIA) extent, which ended around Svalbard at the beginning of the 1920s [45]

  • This study considered research and methodological approaches that may be used for the mapping of glacial landforms

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Summary

Introduction

G EOMORPHOLOGY is an interdisciplinary field studying the distribution, size, morphology, and age of landforms, as well as processes shaping the Earth’s surface. High-resolution satellite-derived or Light Detection And Ranging (LiDAR) digital elevation models (DEMs) form the fundamentals for detailed inspections of terrain attributes to quantitatively and qualitatively describe the Earth’s surface. Novel numerical modeling and machine learning techniques provide reliable and meaningful processing tools for remote sensing datasets, allowing the generation of thematic maps and drawing valuable geomorphological conclusions at various scales [1], [2]. Baker [4] included supervised classification, predictive modeling, and LiDAR mapping as some other trends in future geomorphology development. This article deals with all of the abovementioned disciplines, proposing innovative solutions for glacial geomorphology mapping that may be used worldwide

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