Item type |
紀要論文(ELS) / Departmental Bulletin Paper(1) |
公開日 |
1994-11-01 |
タイトル |
|
|
タイトル |
USING A MOBILE RADIO ECHO SOUNDER TO MEASURE BEDROCK TOPOGRAPHY IN EAST QUEEN MAUD LAND, ANTARCTICA |
言語 |
|
|
言語 |
eng |
資源タイプ |
|
|
資源タイプ識別子 |
http://purl.org/coar/resource_type/c_6501 |
|
資源タイプ |
departmental bulletin paper |
ID登録 |
|
|
ID登録 |
10.15094/00003832 |
|
ID登録タイプ |
JaLC |
ページ属性 |
|
|
内容記述タイプ |
Other |
|
内容記述 |
P(論文) |
論文名よみ |
|
|
その他のタイトル |
USING A MOBILE RADIO ECHO SOUNDER TO MEASURE BEDROCK TOPOGRAPHY IN EAST QUEEN MAUD LAND, ANTARCTICA |
著者名よみ |
マエノ, ヒデオ
カミヤマ, コウキチ
フルカワ, テルオ
ワタナベ, オキツグ
ナルセ, レンジ
オカモト, ケンイチ
スイツ, タケシ
ウラツカ, セイホ
|
著者名(英) |
MAENO, Hideo
KAMIYAMA, Kokichi
FURUKAWA, Teruo
WATANABE, Okitsugu
NARUSE, Renji
OKAMOTO, Kenichi
SUITZ, Takeshi
URATSUKA, Seiho
|
著者所属(英) |
|
|
|
en |
|
|
Communications Research Laboratory |
著者所属(英) |
|
|
|
en |
|
|
National Institute of Polar Research |
著者所属(英) |
|
|
|
en |
|
|
National Institute of Polar Research |
著者所属(英) |
|
|
|
en |
|
|
National Institute of Polar Research |
著者所属(英) |
|
|
|
en |
|
|
Institute of Low Temperature Science, Hokkaido University |
著者所属(英) |
|
|
|
en |
|
|
Communications Research Laboratory |
著者所属(英) |
|
|
|
en |
|
|
Communications Research Laboratory |
著者所属(英) |
|
|
|
en |
|
|
Communications Research Laboratory |
抄録(英) |
|
|
内容記述タイプ |
Other |
|
内容記述 |
As part of the Dome-Fuji Project, the topography of the bedrock over a wide area around Dome-F and along routes from Dome-F to S16 (about 1000 km distance) was surveyed by radio echo sounder with a continuous recording system. The bedrock topography was successfully measured under ice sheets thicker than 3500m, and the performance of the radio echo sounder was confirmed. The highest point of Dome-F was located in the basin like topography of the bedrock, surrounded by more elevated areas. The strength of the bedrock echo were found to differ substantially between inside and outside of the Dome-F area. This difference is probably due to the difference of ice sheet temperatures between these areas, because the attenuation coefficients depend on the ice temperature. The stronger echo at high altitude will enable us to measure ice thickness more than 3500 m. |
雑誌書誌ID |
|
|
収録物識別子タイプ |
NCID |
|
収録物識別子 |
AA10756213 |
書誌情報 |
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
巻 8,
p. 149-160,
発行日 1994-11
|
出版者 |
|
|
出版者 |
National Institute of Polar Research |