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House for Shore: Sentinel-1 reveals Arctic glacier retreat

November 19, 2024
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House for Shore: Sentinel-1 reveals Arctic glacier retreat
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19/11/2024
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As Arctic temperatures rise, marine-terminating glaciers—particularly in locations like Svalbard—are present process speedy retreat and intensified calving.

The ESA-funded House for Shore undertaking utilises radar knowledge from the Copernicus Sentinel-1 mission to supply exact, year-over-year insights into glacier retreat and calving depth, notably in areas like Kongsfjorden, the place notable glaciers are experiencing vital retreat.

Calving, the method of which ice breaks off from a glacier terminus, is a serious contributor to sea-level rise and poses rising dangers to coastal areas worldwide. Understanding these processes, notably within the Arctic, is important for predicting future impacts.

By means of a current part of the Space for Shore project—a collaboration between I-SEA (France) and NORCE (Norway)—scientists have utilised over a thousand picture acquisitions from the Sentinel-1 mission to observe the evolution of Svalbard’s coastal glaciers intimately.

By analysing Sentinel-1 knowledge from 2015 to 2023, the workforce has mapped glacier entrance strains and measured calving exercise throughout Svalbard’s summer time months, when calving intensities are at their highest.

Sentinel-1, a part of the European Union’s Copernicus program, makes use of artificial aperture radar (SAR) know-how to seize high-resolution knowledge underneath difficult Arctic circumstances, making certain constant, year-round monitoring of those essential glaciers.

A key discovering from the evaluation is the yearly extent of glacier fronts. By inspecting photographs captured between July and September, researchers have outlined summer time glacier fronts as areas the place glacier extent is maintained 95% of the time throughout these months.

Moreover, by detecting the radar reflection from floating icebergs and growlers, they’ve developed a proxy for summer time calving depth: summers with larger prevalence of icebergs and growlers—a time period for smaller ice fragments that break off from glaciers—point out extra lively calving and accelerated glacier retreat, that are essential indicators of a glacier’s well being and stability.

Evolution of the Kronebreen glacier

In Kongsfjorden, a key research space, notable glaciers like Kronebreen and Kongsvegen present vital modifications. Within the animation above, the collection of every day Sentinel-1 observations had been used to categorise the area into areas of glacier, iceberg and growler occurence in Kronebukta (Krone Bay) for the summers from 2015 to 2023.

Jörg Haarpaintner, from NORCE, explains, “As an alternative of a snapshot of a glacier entrance place, the Sentinel-1 methodology supplies a statistically outlined composite of the summer time glacier entrance positions and calving intensities, revealing the dynamic interactions between ice and ocean over time.”

Kronebreen glacier entrance

Manon Tranchand, lead researcher on the undertaking, provides, “This evaluation offers us a transparent image of present modifications in Arctic glaciers, and so they’re essential for predicting the long run impacts of local weather change on these delicate areas

“With out the constant, high-resolution knowledge from Sentinel-1, monitoring these dynamic ice-ocean interactions wouldn’t be doable. Ongoing warming is more likely to speed up ice loss, and our knowledge present how that would contribute to world sea-level rise. Sentinel-1’s capabilities permit us to seize these shifts with unprecedented accuracy.”

Wanting forward, the upcoming launch of Sentinel-1C subsequent month marks a major step ahead within the monitoring of Arctic glaciers and world local weather impacts.

As the subsequent addition to the Sentinel-1 mission, Sentinel-1C will present enhanced radar imaging capabilities and improved continuity for essential local weather analysis. With its superior know-how, Sentinel-1C will strengthen our capability to seize detailed, year-round knowledge on glacier entrance strains, calving charges and ice-ocean interactions, even within the difficult circumstances of the Arctic.

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