A model for typhoon track (beta-gyre effect)
- Behavior of a localized vortex on a 2-dimensional barotropic beta plane. Illustration of "beta-gyre effect" explaining a track of typhoons
- A localized votex with differnt strength is placed at the center of the computational domain and its time development is calculated.
- Weak vortex
- The response propagates left-right (east-west).
- Moderate vortex
- The vortex moves left-upward (north-westward).
- Strong vortex
- The vortex moves left (westward) after travelling left-upward (north-westward).
- Weak vortex
- Souce program
- Script for execution. Edit this file in order to modify the experimental paremeters.
For execution of the program,
$ spmfrt plbaro-beta_rn4expcs_betagyre.f90 -o plbaro-beta_rn4expcs_betagyre.out
$ ./plbaro-beta_rn4expcs_betagyre-1.sh