| CASE |
SHORT |
Available Year online (size) |
NOTE |
| f09_g16.E1850C5_IO |
CTL |
Y0021-Y0050 (417G) |
Few variables in output |
| f09_g16.E1850C5_IO_topotest02a |
Arakan |
Y0021-Y0050 (455G) |
The Arakan Yoma is artificially imposed; few variables in output |
| f09_g16.E1850C5_IOn_e02aa |
AA |
Y0021-Y0050 (339G) |
The Arakan Yoma and Annamese Cordillera are artificially imposed |
| f09_g16.E1850C5_IOn_e02z |
IP0 |
Y0021-Y0050 (334G) |
Topography over region (90°E–110°E, 10°N–25°N) is reduced to 100 m |
update: 2022.02.04
- Wu, C. H., W. R. Huang, and S. Y. Wang, 2018: Role of Indochina Peninsula topography in precipitation seasonality over East Asia. Atmosphere 9(7): 255. doi: 10.3390/atmos9070255 (Special Issue Monsoons)
- Wu, C. H., and H. H. Hsu, 2016: Role of the Indochina Peninsula narrow mountains in modulating the East Asia-Western North Pacific summer monsoon. J. Climate, 29, 4445-4459. http://dx.doi.org/10.1175/JCLI-D-15-0594.1
- Wu, C. H., H. H. Hsu, and M. D. Chou, 2014: Effect of the Arakan Mountains in the northwestern Indochina Peninsula on the late May Asian Monsoon transition. J. Geophys. Res. Atmos. 119, 10769-10779. DOI: 10.1002/2014JD022024
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