| Project/Area Number |
23540511
|
|---|
| Research Category |
Grant-in-Aid for Scientific Research (C)
|
| Allocation Type | Multi-year Fund |
|---|
| Section | 一般 |
|---|
| Research Field |
Meteorology/Physical oceanography/Hydrology
|
|---|
| Research Institution | Nagoya University |
|---|
Principal Investigator |
SHINODA Taro 名古屋大学, 地球水循環研究センター, 准教授 (50335022)
|
|---|
| Co-Investigator(Renkei-kenkyūsha) |
TAKEMURA Toshihiko 九州大学, 応用力学研究所, 准教授 (90343326)
|
|---|
| Project Period (FY) |
2011 – 2013
|
| Project Status |
Completed (Fiscal Year 2013)
|
| Budget Amount *help |
¥2,990,000 (Direct Cost: ¥2,300,000、Indirect Cost: ¥690,000)
Fiscal Year 2013: ¥650,000 (Direct Cost: ¥500,000、Indirect Cost: ¥150,000)
Fiscal Year 2012: ¥1,040,000 (Direct Cost: ¥800,000、Indirect Cost: ¥240,000)
Fiscal Year 2011: ¥1,300,000 (Direct Cost: ¥1,000,000、Indirect Cost: ¥300,000)
|
|---|
| Keywords | 水循環 / 大気現象 / エアロゾル |
|---|
| Research Abstract |
We develop a cloud-resolving model including aerosol processes. The aerosol processes of advection, diffusion, gravitational settling, dry deposition, and wet deposition have already been installed. Using the model, we reproduced well the tracing of an aerosol category released from the Fukushima Nuclear Power Plant on March 15, 2011 and the deposition of it on the northern Kanto and Nakadori (Fukushima) regions.
However, we cannot complete the nucleation processes that the aerosol particles act as CCN and/or IN. Although a cloud-resolving model has the two-moment bulk microphysical processes for liquid phase, however, cloud particles cannot develop to raindrops in simple simulations using the model. We are willing to solve the problem after the project finished.
|
