| Project/Area Number |
10041101
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (A).
|
| Allocation Type | Single-year Grants |
|---|
| Section | 一般 |
|---|
| Research Field |
Meteorology/Physical oceanography/Hydrology
|
|---|
| Research Institution | HOKKAIDO UNIVERSITY |
|---|
Principal Investigator |
UYEDA Hiroshi Hokkaido Univ., Grad.School of Sci., Asso.Pro., 大学院・理学研究科, 助教授 (80184935)
|
|---|
| Co-Investigator(Kenkyū-buntansha) |
KAJIKAWA Masahiro Akita Univ., Fac.of Eng.and Resource Sci., Pro., 工学資源学部, 教授 (20042319)
HAYASAKA Tadahiro National Polar Research Institute, Pro., 教授 (40202262)
ASUMA Yoshio Hokkaido Univ., Grad.School of Sci., Lec., 大学院・理学研究科, 講師 (10183732)
KIKUCHI Katsuhiro Akita Prefectural Univ., Fac.of Bioresource Sci., Pro., 生物資源科学部, 教授 (80000793)
WADA Makoto National Polar Research Institute, Asso.Pro., 研究系, 助教授 (40132716)
ソラス M.K. ノルウェー気象局, 北部ノルウェー予報部, 部長
|
|---|
| Project Period (FY) |
1998 – 1999
|
| Project Status |
Completed (Fiscal Year 1999)
|
| Budget Amount *help |
¥8,600,000 (Direct Cost: ¥8,600,000)
Fiscal Year 1999: ¥4,600,000 (Direct Cost: ¥4,600,000)
Fiscal Year 1998: ¥4,000,000 (Direct Cost: ¥4,000,000)
|
|---|
| Keywords | Arctic Region / Arctic Storms / Polar Lows / Polar Meteorology / Mesoscale Meteorology / Cloud Physics / メゾスケール気象学 |
|---|
| Research Abstract |
In order to investigate the water circulation, structures of weather systems, and clouds and precipitation formation mechanism in the Arctic region, ground based observations were carried out using remote sensing instruments in the Scandinavian Arctic region and over the Norwegian Sea.
An X-band vertical pointing Doppler radar was installed at Kiruna, Sweden and collected the data for 4 months from January to April in 1999. It was found that precipitation was strongly affected with the topography of the Scandinavian mountains. To understand the water circulation in this area, it is necessary to understand of the interaction between the topography and weather systems. Meteorological observations were also carried out from October 1999 at Bear Island in the central Norwegian Sea and Ny-Alesund, Spitsbergen. These data set would contribute to understand weather systems and water and energy circulation in the Arctic region.
|
