Automatic digital elevation model (DEM) generation has become an established technique within mapping agencies. This paper assesses the effectiveness of automatic DEM generation using area-based matching for glaciated terrain in Antarctica. DEM accuracy is assessed by comparison with check data acquired using analytical photogrammetry and independent field measurements.An optimum DEM collection strategy is identified. DEM success is linked to ground terrain type and it is found that areas of a DEM which can be collected successfully are relatively insensitive to changes in the collection strategy. A method of isolating unsuccessful areas of a DEM for manual editing is tested for Antarctic terrain. In this example, over 90% success is achiev...
A series of tests on the accuracy of DEMs is described. The effects of four factors on DEM accuracy ...
The need for Digital Elevation Model (DEM) checking has raised since the automated matching techniqu...
Calving Front (CF) is an important parameter to analyse ice sheet dynamics and to measure glacier ma...
Digital Elevation Models (DEMs) are of fundamental importance to a wide range of geoscientific and e...
International audienceA digital elevation model (DEM) was generated using a SPOT5 HRS stereo pair ac...
A high resolution surface topography Digital Elevation Model (DEM) is required to underpin studies o...
The Earth’s topography results from dynamic interactions involving climate, tectonics, and surface p...
In this paper, a new digital elevation model (DEM) is derived for the ice sheet in western Dronning ...
Mertz Glacier (MG) calved in February 2010 and a 70-years’ calving cycle of MG was reported recently...
(ASTER) aboard the Terra satellite was designed to generate along-track stereo images. The data are ...
ABSTRACT: Digital Elevation Models (DEMs) are required for several tasks like generation of orthoima...
The Darwin-Hatherton glacial system is an outlet glacial system in the Transantarctic Mountains, Ant...
The ice shelf is an important component of the Antarctic system, and the interaction between the ice...
A high resolution surface topography Digital Elevation Model (DEM) is required to underpin studies o...
Although accuracy of digital elevation models (DEMs) can be quantified and measured in different way...
A series of tests on the accuracy of DEMs is described. The effects of four factors on DEM accuracy ...
The need for Digital Elevation Model (DEM) checking has raised since the automated matching techniqu...
Calving Front (CF) is an important parameter to analyse ice sheet dynamics and to measure glacier ma...
Digital Elevation Models (DEMs) are of fundamental importance to a wide range of geoscientific and e...
International audienceA digital elevation model (DEM) was generated using a SPOT5 HRS stereo pair ac...
A high resolution surface topography Digital Elevation Model (DEM) is required to underpin studies o...
The Earth’s topography results from dynamic interactions involving climate, tectonics, and surface p...
In this paper, a new digital elevation model (DEM) is derived for the ice sheet in western Dronning ...
Mertz Glacier (MG) calved in February 2010 and a 70-years’ calving cycle of MG was reported recently...
(ASTER) aboard the Terra satellite was designed to generate along-track stereo images. The data are ...
ABSTRACT: Digital Elevation Models (DEMs) are required for several tasks like generation of orthoima...
The Darwin-Hatherton glacial system is an outlet glacial system in the Transantarctic Mountains, Ant...
The ice shelf is an important component of the Antarctic system, and the interaction between the ice...
A high resolution surface topography Digital Elevation Model (DEM) is required to underpin studies o...
Although accuracy of digital elevation models (DEMs) can be quantified and measured in different way...
A series of tests on the accuracy of DEMs is described. The effects of four factors on DEM accuracy ...
The need for Digital Elevation Model (DEM) checking has raised since the automated matching techniqu...
Calving Front (CF) is an important parameter to analyse ice sheet dynamics and to measure glacier ma...