The mechanism of the radiation of the planetary waves by western boundary currents and the driving of the mean flow over a bottom slope.
| Project/Area Number |
21540445
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (C)
|
| Allocation Type | Single-year Grants |
|---|
| Section | 一般 |
|---|
| Research Field |
Meteorology/Physical oceanography/Hydrology
|
|---|
| Research Institution | Hokkaido University |
|---|
Principal Investigator |
MIZUTA Genta 北海道大学, 大学院・地球環境科学研究院, 助教 (30301948)
|
|---|
| Project Period (FY) |
2009 – 2012
|
| Project Status |
Completed (Fiscal Year 2012)
|
| Budget Amount *help |
¥4,160,000 (Direct Cost: ¥3,200,000、Indirect Cost: ¥960,000)
Fiscal Year 2012: ¥910,000 (Direct Cost: ¥700,000、Indirect Cost: ¥210,000)
Fiscal Year 2011: ¥1,170,000 (Direct Cost: ¥900,000、Indirect Cost: ¥270,000)
Fiscal Year 2010: ¥910,000 (Direct Cost: ¥700,000、Indirect Cost: ¥210,000)
Fiscal Year 2009: ¥1,170,000 (Direct Cost: ¥900,000、Indirect Cost: ¥270,000)
|
|---|
| Keywords | 地球流体力学 / ジェット / ロスビー波 / 海底地形 / 波による平均流形成 / 海洋物理・陸水学 |
|---|
| Research Abstract |
The dynamics of the interaction between the planetary waves, which are radiated from an ocean jet such as the Kuroshio Extension, the large-scale mean flow, and bottom topography is examined. It is shown that the planetary waves broadens the jet and matches it with weak flows in the ocean interior. The planetary waves also induce the equatorward potential-vorticity flux in the abyss, driving deep recirculations. After impinging over a bottom slope of seamounts, trenches, etc, the planetary waves induce the mean flow that is trapped near both the bottom and surface.
|
Report
(5 results)
Research Products
(4 results)
