Preprints
https://doi.org/10.5194/gchron-2022-18
https://doi.org/10.5194/gchron-2022-18
 
03 Aug 2022
03 Aug 2022
Status: a revised version of this preprint was accepted for the journal GChron and is expected to appear here in due course.

Technical note: Evaluating a geographical information system (GIS)- based approach for determining topographic shielding factors in cosmic-ray exposure dating

Felix Martin Hofmann Felix Martin Hofmann
  • Institute of Earth and Environmental Sciences, University of Freiburg, Freiburg, 79104, Germany

Abstract. Cosmic-ray exposure (CRE) dating of boulders on terminal moraines has become a well-established technique to reconstruct glacier chronologies. If topographical obstructions are present in the surroundings of sampling sites, CRE ages need to be corrected for topographic shielding. In recent years, geographical information system (GIS)-based approaches have been developed to compute shielding factors with elevation data, particularly two toolboxes for the ESRI ArcGIS software. So far, the output of the most recent toolbox (Li, 2018) has only been validated with a limited number of field data-based shielding factors. Additionally, it has not been systematically evaluated how the spatial resolution of the input-elevation data affects the output of the toolbox and whether a correction for vegetation leads to considerably more precise shielding factors. This paper addresses these issues by assessing the output of the toolbox with an extensive set of field data-based shielding factors. Commonly used elevation data with different spatial resolutions were tested as input. To assess the impact of the different methods on CRE ages, ages of boulders at three sites with different topography were first recalculated with GIS-based and then with field data-based shielding factors. For sampling sites in forested low mountainous areas and in high Alpine settings, the shielding factors were stable, i.e. independent of the spatial resolution of the input-elevation data. Vegetation-corrected elevation data allowed more precise shielding factors to be computed for sites in a forested low mountainous area. In most cases, recalculating CRE ages with different shielding factors for the same sampling sites led to minor changes in ages. Only in a few cases, the shifts were in the order of a few percent. It is shown that the use of elevation data with a very high resolution requires precise xy-coordinates of sampling sites. Otherwise, there is a risk that small-scale objects in the vicinity of sampling sites will be misinterpreted as topographic barriers. Overall, the toolbox provides an interesting avenue for the determination of shielding factors. Together with the guidelines presented here, it should be more widely used.

Felix Martin Hofmann

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on gchron-2022-18', Yingkui Li, 19 Aug 2022
    • AC1: 'Reply on RC1', Felix Martin Hofmann, 25 Oct 2022
  • RC2: 'Comment on gchron-2022-18', Michal Ben-Israel, 22 Sep 2022
    • AC2: 'Reply on RC2', Felix Martin Hofmann, 25 Oct 2022

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on gchron-2022-18', Yingkui Li, 19 Aug 2022
    • AC1: 'Reply on RC1', Felix Martin Hofmann, 25 Oct 2022
  • RC2: 'Comment on gchron-2022-18', Michal Ben-Israel, 22 Sep 2022
    • AC2: 'Reply on RC2', Felix Martin Hofmann, 25 Oct 2022

Felix Martin Hofmann

Felix Martin Hofmann

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Short summary
If topographical obstructions are present in the surroundings of sampling sites, exposure ages of rock surfaces need to be corrected. A toolbox for the ESRI ArcGIS software allows for quantifying topographic shielding with a digital elevation model, but it has only been validated with few field data. In this study, the output of the toolbox is evaluated with a more extensive dataset. If suitable elevation data is chosen, the toolbox provides a sound approach to determine topographic shielding.