The Cryosphere (Nov 2024)

The Pléiades Glacier Observatory: high-resolution digital elevation models and ortho-imagery to monitor glacier change

  • E. Berthier,
  • E. Berthier,
  • J. Lebreton,
  • D. Fontannaz,
  • S. Hosford,
  • J. M.-C. Belart,
  • F. Brun,
  • L. M. Andreassen,
  • B. Menounos,
  • B. Menounos,
  • B. Menounos,
  • C. Blondel

DOI
https://doi.org/10.5194/tc-18-5551-2024
Journal volume & issue
Vol. 18
pp. 5551 – 5571

Abstract

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Spaceborne digital elevation models (DEMs) of glaciers are essential to describe their health and their contribution to river runoff and sea level rise. Publicly available DEMs derived from sub-meter satellite stereo imagery were, up to now, mainly available in the polar regions and High Mountain Asia. Here, we present the Pléiades Glacier Observatory (PGO), a scientific program acquiring Pléiades 0.7 m satellite stereo pairs for 140 sites from Earth's glacierized areas. The PGO product consists of freely available DEMs at 2 and 20 m ground sampling distance together with 0.5 m (panchromatic) and 2 m (multispectral) ortho-images. PGO stereo acquisitions began in July 2016 in the Northern Hemisphere and February 2017 in the Southern Hemisphere. Each site is revisited every 5 years (cloud permitting), close to the end of the melt season, to measure glacier elevation change with an average uncertainty of 0.49 m (95 % confidence level, for a glacierized area of 1 km2), i.e., 0.1 m yr−1. PGO samples over 20 000 km2 of glacierized terrain, which represents about 3 % of the Earth's glacier area. This small sample, however, provides a first-order estimate (within 0.07 mw.e.yr-1) of the global glacier mass change and its decadal evolution.