Abstract

Observing changes in Earth surface topography is crucial for many Earth science disciplines. Documenting these changes over several decades at regional to global scale remains a challenge due to the limited availability of suitable satellite data before the year 2000. Declassified analog satellite images from the American reconnaissance program Hexagon (KH-9), which surveyed nearly all land surfaces from 1972 to 1986 at metric resolution, provide a unique opportunity to fill the gap in observations. However, large-scale processing of analog imagery remains challenging. We developed an automated workflow to generate Digital Elevation Models (DEMs) and orthophotos from scanned KH-9 mapping camera stereo images. The workflow includes a preprocessing step to correct for film and scanning distortions and crop the scanned images, and a stereo reconstruction step using the open-source NASA Ames Stereo Pipeline. The processing of several hundreds of image pairs enabled us to estimate reliable camera parameters for each KH-9 mission, thereby correcting elevation biases of several tens of meters. The resulting DEMs were validated against various reference elevation data, including snow-covered glaciers with limited image texture. Pixel-scale elevation uncertainty was estimated as 5 m at the 68% confidence level, and less than 15 m at the 95% level. We evaluated the uncertainty of spatially averaged elevation change and volume change, both from an empirical and analytical approach, and we raise particular attention to large-scale correlated biases that may impact volume change estimates from such DEMs. Finally, we present a case study of long-term glacier elevation change in the European Alps. Our results show the suitability of these historical images to quantitatively study global surface change over the past 40-50 years.

Highlights

  • The Earth’s surface has evolved dramatically over the last century as a consequence of anthropogenic activities and climate change (IPCC, 2019; IPCC SROC, 2019)

  • We presented ASPy, an automated workflow to generate Digital Elevation Models (DEMs) from analog Hexagon (KH-9) mapping camera images, which covered most of Earth’s land surface between 1973 and 1980

  • The processing uses the crude image geolocation provided by the USGS and an external DEM to avoid the labor-intensive process of manually identifying Ground Control Points (GCPs)

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Summary

Introduction

The Earth’s surface has evolved dramatically over the last century as a consequence of anthropogenic activities and climate change (IPCC, 2019; IPCC SROC, 2019). Documenting these changes at regional scales over such a time span remains a challenge (James et al, 2012). Prior to the Shuttle Radar Topography Mission (SRTM) in 2000, no elevation data are available at a global scale with the decameter resolution required to study Earth surface deformation. A potential source of data to fill in the temporal gap is declassified American intelligence satellite imagery, such as from the Corona and Hexagon programs (Galiatsatos et al, 2007; Burnett, 2012; Fowler, 2013).

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