This paper summarizes the progress of the Chinese Antarctic expedition in geodetic remote sensing. It describes the systems for continuous satellite navigation and positioning, and the tide gauges that have been established at the Zhongshan and Great Wall stations in Antarctica. Advances in the investigation of plate motion, the gravity field, and sea level change as well as the application of GPS in atmospheric studies are reported. Details of the movements of ice sheets and glaciers, distributions of blue ice and ice crevasses, and mass balance studies based on remote sensing techniques are presented. The use of field, satellite, and photogrammetric data to produce topographic maps is described. Finally, the prospects for further Antarcti...
The Antarctic geomagnetics community remains very active in crustal anomaly mapping. Several interna...
This paper includes a short historical review of Russian and Soviet scientific traverses to study th...
In order to study geodynamics in relation to atmospheric, oceanographic and glaciological interactio...
Marine geophysical survey by the Chinese National Antarctic Research Expedition (CHINARE) began with...
Chinese radioglaciological studies on the Antarctic ice sheet (AIS) began in 2004/05 when the 21st C...
By 2018, China had conducted 34 scientific explorations in Antarctica spearheaded by the Chinese Nat...
It is more than 30 years since the first Chinese National Antarctic Research Expedition (CHINARE) la...
The highest part of the East Antarctic Ice Sheet, more than 4000 m above sea level, has been an area...
Within the context of developing a research presence in the Antarctic region, the first phase of the...
The polar regions with their unique geophysical and geodynamic environment are characterized by clos...
The 1228 km over-snow traverse route between the Chinese Zhongshan Station, on the coast of Prydz Ba...
Modern geodetic technologies, including high-precision ground-based gravity measurements, satellite ...
The Antarctic Peninsula has undergone dramatic changes in recent decades, including ice-shelf meltin...
It has been more than 30 years since the first Chinese Antarctic Expedition took place. Polar upper ...
Cold regions, including high-latitude and high-altitude landscapes, are experiencing profound envir...
The Antarctic geomagnetics community remains very active in crustal anomaly mapping. Several interna...
This paper includes a short historical review of Russian and Soviet scientific traverses to study th...
In order to study geodynamics in relation to atmospheric, oceanographic and glaciological interactio...
Marine geophysical survey by the Chinese National Antarctic Research Expedition (CHINARE) began with...
Chinese radioglaciological studies on the Antarctic ice sheet (AIS) began in 2004/05 when the 21st C...
By 2018, China had conducted 34 scientific explorations in Antarctica spearheaded by the Chinese Nat...
It is more than 30 years since the first Chinese National Antarctic Research Expedition (CHINARE) la...
The highest part of the East Antarctic Ice Sheet, more than 4000 m above sea level, has been an area...
Within the context of developing a research presence in the Antarctic region, the first phase of the...
The polar regions with their unique geophysical and geodynamic environment are characterized by clos...
The 1228 km over-snow traverse route between the Chinese Zhongshan Station, on the coast of Prydz Ba...
Modern geodetic technologies, including high-precision ground-based gravity measurements, satellite ...
The Antarctic Peninsula has undergone dramatic changes in recent decades, including ice-shelf meltin...
It has been more than 30 years since the first Chinese Antarctic Expedition took place. Polar upper ...
Cold regions, including high-latitude and high-altitude landscapes, are experiencing profound envir...
The Antarctic geomagnetics community remains very active in crustal anomaly mapping. Several interna...
This paper includes a short historical review of Russian and Soviet scientific traverses to study th...
In order to study geodynamics in relation to atmospheric, oceanographic and glaciological interactio...