Geoscience Reference
In-Depth Information
mainly due to the non-uniform SSTA effect. The decreased vertical wind shear
seems to be responsible for the increase in TC frequency in the Arabian Sea,
while the increased upward mass flux associated with the enhanced precipitation
is responsible for the increase in TC frequency in the South Indian Ocean.
Acknowledgement
This work was conducted under the framework of the “Projection of the Change
in future Weather Extremes using Super-high-resolution Atmospheric Models”
supported by the KAKUSHIN Program of the Ministry of Education, Culture,
Sports, Science, and Technology (MEXT). The calculations were performed
on the Earth Simulator.
REFERENCES
Held, I.M. and Zhao, M. (2011). The response of tropical cyclone statistics to an increase
in CO 2 with fixed sea surface temperature. J. Clim. , 24: 5353-5364, doi:10.1175/
JCLI-D-11-00050.1.
Knutson, T., McBride, J., Chan, J., Emanuel, K., Holland, G., Landsea, C., Held, I.,
Kossin, J.P., Srivastava, A. and Sugi, M. (2010). Tropical cyclones and climate
change. Nature Geoscience , doi:10.1038/ngeo0779.
Mizuta, R., Yoshimura, H., Murakami, H., Matsueda, M., Endo, H., Ose, T., Kamiguchi,
K., Hosaka, M., Sugi, M., Yukimoto, S., Kusunoki, S. and Kitoh, A. (2012). Climate
simulations using MRI-AGCM with 20-km grid. J. Meteor. Soc. Japan , 90A: 233-
258.
Murakami, H., Mizuta, R. and Shindo, E. (2012a). Future changes in tropical cyclone
activity projected by multi-model and multi-SST ensemble experiments using 60-
km mesh MRI-AGCM. Clim. Dyn., Doi 10.1007/s00382-011-1223-x.
Murakami, H., Sugi, M. and Kitoh, A. (2012b). Future changes in tropical cyclone
activity in the North Indian Ocean projected by high-resolution MRI-AGCMs.
Clim. Dyn., Doi 10.1007/s00382-012-1407-z.
Sugi, M., Noda, A. and Sato, N. (2002). Influence of the global warming on tropical
cyclone climatology: An experiment with the JMA global model. J. Meteorol. Soc.
Japan ., 80: 249-272, doi:10.2151/jmsj.80.249.
Sugi, M. and Yoshimura, J. (2004). A mechanism of tropical precipitation change due
to CO 2 increase. J. Climate , 17: 238-243.
Sugi, M., Murakami, H. and Yoshimura, J. (2009). A reduction in global tropical cyclone
frequency due to global warming. SOLA , 5: 164-167.
Sugi, M., Murakami, H. and Yoshimura, J. (2012). On the mechanism of tropical cyclone
frequency change due to global warming. J. Meteor. Soc. Japan , 90A: 399-410.
Sugi, M. and Yoshimura, J. (2012). Decreasing trend of tropical cyclone frequency in
228-year high-resolution AGCM simulations. Geophys. Res. Lett. , 39: L19805,
doi:10.1029/2012GL053360.
Yoshimura, J. and Sugi, M. (2005). Tropical cyclone climatology in a high resolution
AGCM—Impacts of SST warming and CO 2 increase. SOLA , 1: 133-136.
Search WWH ::




Custom Search