Potential of the Bi-Static SAR Satellite Companion Mission Harmony for Land-Ice Observations

Journal Article (2024)
Author(s)

Andreas Kääb (Universitetet i Oslo)

Jérémie Mouginot (Université Grenoble Alpes)

Pau Prats-Iraola (Deutsches Zentrum für Luft- und Raumfahrt (DLR))

Eric Rignot (University of California)

Bernhard Rabus (Simon Fraser University)

Andreas Benedikter (Deutsches Zentrum für Luft- und Raumfahrt (DLR))

Helmut Rott (ENVEO Environmental Earth Observation IT GmbH)

Thomas Nagler (ENVEO Environmental Earth Observation IT GmbH)

Bjorn Rommen (European Space Agency (ESA))

Francisco Dekker (TU Delft - Mathematical Geodesy and Positioning)

Research Group
Mathematical Geodesy and Positioning
DOI related publication
https://doi.org/10.3390/rs16162918
More Info
expand_more
Publication Year
2024
Language
English
Research Group
Mathematical Geodesy and Positioning
Issue number
16
Volume number
16
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

The EarthExplorer 10 mission Harmony by the European Space Agency ESA, scheduled for launch around 2029–2030, consists of two passive C-band synthetic-aperture-radar companion satellites flying in a flexible constellation with one Sentinel-1 radar satellite as an illuminator. Sentinel-1 will serve as transmitter and receiver of radar waves, and the two Harmonys will serve as bistatic receivers without the ability to transmit. During the first and last year of the 5-year mission, the two Harmony satellites will fly in a cross-track interferometric constellation, such as that known from TanDEM-X, about 350 km ahead or behind the assigned Sentinel-1. This constellation will provide 12-day repeat DEMs, among other regions, over most land-ice and permafrost areas. These repeat DEMs will be complemented by synchronous lateral terrain displacements from the well-established offset tracking method. In between the cross-track interferometry phases, one of the Harmony satellites will be moved to the opposite side of the Sentinel-1 to form a symmetric bistatic “stereo” constellation with ±~350 km along-track baseline. In this phase, the mission will provide opportunity for radar interferometry along three lines of sight, or up to six when combining ascending and descending acquisitions, enabling the measurement of three-dimensional surface motion, for instance sub- and emergence components of ice flow, or three-dimensional deformation of permafrost surfaces or slow landslides. Such measurements would, for the first time, be available for large areas and are anticipated to provide a number of novel insights into the dynamics and mass balance of a range of mass movement processes.