Gravity measurements on board the icebreaker SHIRASE have been conducted during the 33rd Japanese Antarctic Research Expedition (JARE-33). Although the purposes and the procedure for the gravity measurements are essentially the same as for previous expeditions, we have made mainly two improvements on the measuring system as follows. The first modification is the improvement of the online data acquisition and data processing system, aiming at fully automatic measurement. While a mini-computer was used for processing in the previous system, two personal computers, which share the tasks, are employed in the present system. This down-sizing improves the total system reliability and decreases maintenance. The second improvement is the employment...
A newly-designed ship-borne gravimeter NIPR-ORI Model II to be used for the Japanese Antarctic Resea...
Gravity survey was carried out in Cape Ryugu, and East and West Ongul Islands by the summer party of...
Gravity anomalies and geoidal undulations around the Japanese Antarctic stations (60°-80°S, 20°-50°E...
Since the advent of icebreaker SHIRASE for Antarctic research in 1983,the gravity measurements have ...
Sea gravity measurements on board the icebreaker SHIRASE were continuously conducted during the 27th...
The NIPRORI-1 gravimeter of icebreaker SHIRASE was modified so that the ship\u27s navigational data ...
Sea gravity measurements on board the icebreaker FUJI in the Antarctic regions were conducted in the...
Gravity value at Astronomical point, Syowa station, was determined by observations with a WORDEN gra...
To compile consistent data sets of Japanese Antarctic Research Expedition (JARE) shipborne gravity d...
The gravimeter system of the SHIRASE is the NIPRORI-1 sea gravimeter which was transferred from the ...
Recent techniques of marine gravimetry and gravimeters available are reviewed and some requirements ...
Abstract The gravity field is one of the Earth’s basic physical fields. The geoid can be calculated ...
The Ninth Symposium on Polar Science/Ordinary sessions: [OG] Polar Geosciences, Wed. 5 Dec. / Entran...
Gravimetric connection between Asuka Camp and Syowa Station was established during the summer activi...
Sea gravity measurements on board the icebreaker FUJI during the 22nd Japanese Antarctic Research Ex...
A newly-designed ship-borne gravimeter NIPR-ORI Model II to be used for the Japanese Antarctic Resea...
Gravity survey was carried out in Cape Ryugu, and East and West Ongul Islands by the summer party of...
Gravity anomalies and geoidal undulations around the Japanese Antarctic stations (60°-80°S, 20°-50°E...
Since the advent of icebreaker SHIRASE for Antarctic research in 1983,the gravity measurements have ...
Sea gravity measurements on board the icebreaker SHIRASE were continuously conducted during the 27th...
The NIPRORI-1 gravimeter of icebreaker SHIRASE was modified so that the ship\u27s navigational data ...
Sea gravity measurements on board the icebreaker FUJI in the Antarctic regions were conducted in the...
Gravity value at Astronomical point, Syowa station, was determined by observations with a WORDEN gra...
To compile consistent data sets of Japanese Antarctic Research Expedition (JARE) shipborne gravity d...
The gravimeter system of the SHIRASE is the NIPRORI-1 sea gravimeter which was transferred from the ...
Recent techniques of marine gravimetry and gravimeters available are reviewed and some requirements ...
Abstract The gravity field is one of the Earth’s basic physical fields. The geoid can be calculated ...
The Ninth Symposium on Polar Science/Ordinary sessions: [OG] Polar Geosciences, Wed. 5 Dec. / Entran...
Gravimetric connection between Asuka Camp and Syowa Station was established during the summer activi...
Sea gravity measurements on board the icebreaker FUJI during the 22nd Japanese Antarctic Research Ex...
A newly-designed ship-borne gravimeter NIPR-ORI Model II to be used for the Japanese Antarctic Resea...
Gravity survey was carried out in Cape Ryugu, and East and West Ongul Islands by the summer party of...
Gravity anomalies and geoidal undulations around the Japanese Antarctic stations (60°-80°S, 20°-50°E...