Automatic delineation of cracks with Sentinel-1 interferometry for monitoring ice shelf damage and calving
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Published:2022-04-27
Issue:4
Volume:16
Page:1523-1542
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ISSN:1994-0424
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Container-title:The Cryosphere
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language:en
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Short-container-title:The Cryosphere
Author:
Libert Ludivine, Wuite JanORCID, Nagler ThomasORCID
Abstract
Abstract. Monitoring the evolution of ice shelf damage such as
crevasses and rifts is important for a better understanding of the
mechanisms controlling the breakup of ice shelves and for improving
predictions about iceberg calving and ice shelf disintegration. Nowadays,
the previously existing observational gap has been reduced by the Copernicus
Sentinel-1 synthetic aperture radar (SAR) mission that provides a continuous
coverage of the Antarctic margins with a 6 or 12 d repeat period. The
unprecedented coverage and temporal sampling enables, for the first time, a
year-round systematic monitoring of ice shelf fracturing and iceberg
calving, as well as the detection of precursor signs of calving events. In
this paper, a novel method based on SAR interferometry is presented for an
automatic detection and delineation of active cracks on ice shelves.
Propagating cracks cause phase discontinuities that are extracted
automatically by applying a Canny edge detection procedure to the spatial
phase gradient derived from a SAR interferogram. The potential of the
proposed method is demonstrated in the case of Brunt Ice Shelf, Antarctica,
using a stack of 6 d repeat-pass Sentinel-1 interferograms acquired
between September 2020 and March 2021. The full life cycle of the North Rift
is monitored, including the rift detection, its propagation at rates varying
between 0.25 and 1.30 km d−1, and the final calving event
that gave birth to the iceberg A74 on 26 February 2021. The automatically
delineated cracks agree well with the North Rift location in Landsat 8
images and with the eventual location of the ice shelf edge after the
iceberg broke off. The strain variations observed in the interferograms are
attributed to a rigid-body rotation of the ice about the expanding tip of
the North Rift in response to the rifting activity. The extent of the North
Rift is captured by SAR interferometry well before it becomes visible in SAR
backscatter images and a few days before it could be identified in optical
images, hence highlighting the high sensitivity of SAR interferometry to
small variations in the ice shelf strain pattern and its potential for
detecting early signs of natural calving events, ice shelf fracturing and
damage development.
Funder
European Space Agency
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
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