Project/Area Number |
15310017
|
Research Category |
Grant-in-Aid for Scientific Research (B)
|
Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Environmental dynamic analysis
|
Research Institution | National Institute of Polar Research |
Principal Investigator |
FURUKAWA Teruo National Institute of Polar Research, Division for Research and Education, Research Assistant, 研究教育系, 助手 (70261120)
|
Co-Investigator(Kenkyū-buntansha) |
FUIJI Yoshiyuki National Institute of Polar Research, Director General, 所長 (20125214)
MOTOYAMA Hideaki National Institute of Polar Research, Division for Research and Education, Associate Professor, 研究教育系, 助教授 (20210099)
FUJITA Shuji National Institute of Polar Research, Division for Research and Education, Associate Professor, 研究教育系, 助教授 (30250476)
NISHIO Fumihiko Chiba University, Center for Environmental Remote Sensing, Professor, 環境リモートセンシング研究センター, 教授 (40044789)
松岡 健一 総合地球環境学研究所, 日本学術振興会特別研究員
|
Project Period (FY) |
2003 – 2005
|
Project Status |
Completed (Fiscal Year 2005)
|
Budget Amount *help |
¥9,700,000 (Direct Cost: ¥9,700,000)
Fiscal Year 2005: ¥1,300,000 (Direct Cost: ¥1,300,000)
Fiscal Year 2004: ¥2,900,000 (Direct Cost: ¥2,900,000)
Fiscal Year 2003: ¥5,500,000 (Direct Cost: ¥5,500,000)
|
Keywords | Synthetic Aperture Radar(SAR) / Antarctica / ice sheet / the end of ice sheet / global climatic change / change in ice sheet / Geographic Information System (GIS) |
Research Abstract |
It is important to reveal the variation in ice mass of the Antarctic ice sheet caused by global climatic change. The objective of this project is to reveal the effect of variation in the end of ice sheet on the dynamical behavior of drainage basin in Antarctic ice sheet. Japanese Antarctic Research Expeditions (JAREs) have collected the ground data on surface topography, bedrock topography, surface snow conditions and surface mass balance in the Shirase drainage basin of which summit of the ice sheet (Dome Fuji). The dynamical behavior of Shirase Glacier is very important to understand the response of the Shirase drainage basin to global climatic change. It is difficult to approach Shirase Glacier because of the existence of many crevasses. It is possible to collect various information of the glacier using Synthetic Aperture Radar (SAM). In order to investigate the effect of variation of the end of ice sheet on the dynamical behavior of drainage basin in Antarctica, the analysis system was built using Geographic Information System (GIS). It is possible to compare ground observation data such as surface topography, snow surface conditions and surface mass balance with image data by Synthetic Aperture Radar (SAR). And to reveal the mechanism of ice sheet change, the analysis of multi frequencies radio echo sounding observation data on the internal structure of the ice sheet.
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