Code, models, and results for the paper "A Benchmark Dataset and Methodology for Automatic Glacier Calving Front Extraction from SAR Imagery". Abstract Exact information on calving front positions of marine- or lake-terminating glaciers is a fundamental glacier variable for analyzing ongoing glacier change processes and assessing other variables like frontal ablation rates. In recent years, researchers started implementing algorithms that could automatically detect the calving fronts on satellite imagery. Most studies use optical images, as in these images, calving fronts are often easy to distinguish due to sufficient spatial resolution and the presence of different spectral bands, allowing the separation of ice features. However, detecti...
The extent of Antarctic ice shelves and glacier tongues is important for accurate sea level rise pre...
We present a deep active contour model for detecting and delineating glacier calving fronts from sat...
Antarctica’s coastline is constantly changing due to fluctuations in glacier and ice shelf front pos...
The temporal variability in calving front positions of marine-terminating glaciers permits inference...
This paper presents an approach for automatic calving front delineation of marine-terminating outle...
Antarctic glacier termini and ice shelf fronts are sensitive indicators of glaciological and environ...
Glacier calving front position (CFP) is an important glaciological variable. Traditionally, delineat...
The continuous and precise mapping of glacier calving fronts is essential for monitoring and underst...
The continuous and precise mapping of glacier calving fronts is essential for monitoring and underst...
An accurate parameterization of glacier calving is essential for understanding glacier dynamics and ...
Sea level rise contribution from the Antarctic ice sheet is influenced by changes in glacier and ice...
Changes in the calving front position of marine-terminating glaciers strongly influence the mass bal...
The Antarctic ice sheet stores ~91% of the global ice volume which is equivalent to a sea-level rise...
Calving is an important process in glacier systems terminating in the ocean, and more observations a...
Extents of Antarctica`s ice shelves and ice streams are sensitive indicators of glaciological and en...
The extent of Antarctic ice shelves and glacier tongues is important for accurate sea level rise pre...
We present a deep active contour model for detecting and delineating glacier calving fronts from sat...
Antarctica’s coastline is constantly changing due to fluctuations in glacier and ice shelf front pos...
The temporal variability in calving front positions of marine-terminating glaciers permits inference...
This paper presents an approach for automatic calving front delineation of marine-terminating outle...
Antarctic glacier termini and ice shelf fronts are sensitive indicators of glaciological and environ...
Glacier calving front position (CFP) is an important glaciological variable. Traditionally, delineat...
The continuous and precise mapping of glacier calving fronts is essential for monitoring and underst...
The continuous and precise mapping of glacier calving fronts is essential for monitoring and underst...
An accurate parameterization of glacier calving is essential for understanding glacier dynamics and ...
Sea level rise contribution from the Antarctic ice sheet is influenced by changes in glacier and ice...
Changes in the calving front position of marine-terminating glaciers strongly influence the mass bal...
The Antarctic ice sheet stores ~91% of the global ice volume which is equivalent to a sea-level rise...
Calving is an important process in glacier systems terminating in the ocean, and more observations a...
Extents of Antarctica`s ice shelves and ice streams are sensitive indicators of glaciological and en...
The extent of Antarctic ice shelves and glacier tongues is important for accurate sea level rise pre...
We present a deep active contour model for detecting and delineating glacier calving fronts from sat...
Antarctica’s coastline is constantly changing due to fluctuations in glacier and ice shelf front pos...