Abstract

The availability of global digital elevation models (DEMs) from multiple time points allows their combination for analysing vegetation changes. The combination of models (e.g., SRTM and TanDEM-X) can contain errors, which can, due to their synergistic effects, yield incorrect results. We used a high-resolution LiDAR-derived digital surface model (DSM) to evaluate the accuracy of canopy height estimates of the aforementioned global DEMs. In addition, we subtracted SRTM and TanDEM-X data at 90 and 30 m resolutions, respectively, to detect deforestation caused by bark beetle disturbance and evaluated the associations of their difference with terrain characteristics. The study areas covered three Central European mountain ranges and their surrounding areas: Bohemian Forest, Erzgebirge, and Giant Mountains. We found that vertical bias of SRTM and TanDEM-X, relative to the canopy height, is similar with negative values of up to −2.5 m and LE90s below 7.8 m in non-forest areas. In forests, the vertical bias of SRTM and TanDEM-X ranged from −0.5 to 4.1 m and LE90s from 7.2 to 11.0 m, respectively. The height differences between SRTM and TanDEM-X show moderate dependence on the slope and its orientation. LE90s for TDX-SRTM differences tended to be smaller for east-facing than for west-facing slopes, and varied, with aspect, by up to 1.5 m in non-forest areas and 3 m in forests, respectively. Finally, subtracting SRTM and NASA DEMs from TanDEM-X and Copernicus DEMs, respectively, successfully identified large areas of deforestation caused by hurricane Kyril in 2007 and a subsequent bark beetle disturbance in the Bohemian Forest. However, local errors in TanDEM-X, associated mainly with forest-covered west-facing slopes, resulted in erroneous identification of deforestation. Therefore, caution is needed when combining SRTM and TanDEM-X data in multitemporal studies in a mountain environment. Still, we can conclude that SRTM and TanDEM-X data represent suitable near global sources for the identification of deforestation in the period between the time points of their acquisition.

Highlights

  • We evaluated two global digital elevation models (DEMs) produced using radar interferometry (SRTM and TanDEM-X) in three Central European mountain ranges

  • A comparison of SRTM and TanDEM-X 90m DEM with LiDAR digital surface model (DSM) showed that both models tend to underestimate the canopy height by several meters

  • Our analysis shows that differences of SRTM and TanDEM-X show a moderate dependence on terrain characteristics

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Summary

Introduction

Computers and remote sensing drove innovations in Earth surface observation. Data availability has been continuously growing, including surface observation data at a variety of scales [1]. Synthetic Aperture Radar (SAR) sensors are commonly used for mapping Earth’s surface, due to their capability of mapping large areas within a short time and due to the fact that they are almost independent of weather conditions (i.e., they penetrate clouds, smoke, fog, and rain). Several SAR satellite systems have been operating in the last two decades [2]. SAR sensors were, for example, on Remote Sens.

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