Calving Front (CF) is an important parameter to analyse ice sheet dynamics and to measure glacier mass balance. DEM products covering polar regions are critical remote sensing data sources to provide fundamental terrain information for glaciological studies. It is necessary to provide accurate CFs for DEM specific applications, such as mass balance calculation or the substitution of water values with geoid values in the DEM editing process. However, much less attention is paid to automatically delineate CFs from DEM data. In this study, we propose a DEM-based Automatic CF Extraction method (DACE) to efficiently extract the CFs from DEM data. In DACE, a height-sensitive terrain feature is designed to enhance the contrast between the ice shee...
Antarctic glacier termini and ice shelf fronts are sensitive indicators of glaciological and environ...
Ice shelf calving is an important mass loss component of the Antarctic Ice Sheet (AIS). The discharg...
Iceberg calving is the largest loss term in Antarctic mass balance. The iceberg areas vary from a fe...
The temporal variability in calving front positions of marine-terminating glaciers permits inference...
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...
This paper presents an approach for automatic calving front delineation of marine-terminating outle...
Mertz Glacier (MG) calved in February 2010 and a 70-years’ calving cycle of MG was reported recently...
Antarctica’s coastline is constantly changing due to fluctuations in glacier and ice shelf front pos...
Code, models, and results for the paper "A Benchmark Dataset and Methodology for Automatic Glacier C...
The Earth’s topography results from dynamic interactions involving climate, tectonics, and surface p...
Automatic digital elevation model (DEM) generation has become an established technique within mappin...
Mapping the time-variable calving front location (CFL) of Antarctic ice shelves is important for est...
Extents of Antarctica`s ice shelves and ice streams are sensitive indicators of glaciological and en...
In this paper, a new digital elevation model (DEM) is derived for the ice sheet in western Dronning ...
Antarctic glacier termini and ice shelf fronts are sensitive indicators of glaciological and environ...
Ice shelf calving is an important mass loss component of the Antarctic Ice Sheet (AIS). The discharg...
Iceberg calving is the largest loss term in Antarctic mass balance. The iceberg areas vary from a fe...
The temporal variability in calving front positions of marine-terminating glaciers permits inference...
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...
This paper presents an approach for automatic calving front delineation of marine-terminating outle...
Mertz Glacier (MG) calved in February 2010 and a 70-years’ calving cycle of MG was reported recently...
Antarctica’s coastline is constantly changing due to fluctuations in glacier and ice shelf front pos...
Code, models, and results for the paper "A Benchmark Dataset and Methodology for Automatic Glacier C...
The Earth’s topography results from dynamic interactions involving climate, tectonics, and surface p...
Automatic digital elevation model (DEM) generation has become an established technique within mappin...
Mapping the time-variable calving front location (CFL) of Antarctic ice shelves is important for est...
Extents of Antarctica`s ice shelves and ice streams are sensitive indicators of glaciological and en...
In this paper, a new digital elevation model (DEM) is derived for the ice sheet in western Dronning ...
Antarctic glacier termini and ice shelf fronts are sensitive indicators of glaciological and environ...
Ice shelf calving is an important mass loss component of the Antarctic Ice Sheet (AIS). The discharg...
Iceberg calving is the largest loss term in Antarctic mass balance. The iceberg areas vary from a fe...