associated with sea surface temperature change in the tropical Pacific. J. Meteor. Soc. Japan, 89, 539–552.

37) Kusunoki, S. and O. Arakawa (2011): Change in the precipitation intensity of the East Asian summer monsoon projected by CMIP3 models. Climate Dynamics, doi 10.1007/s00382-011-1234-7.

38) Tanimoto, Y., T. Kanenari, H. Tokinaga, and S.-P. Xie (2011): Sea level pressure minimum along the Kuroshio and its extension. J. Climate, 24, 4419–4434, doi:10.1175/2011JCLI4062.1.

39) Inoue, T. and H. Ueda (2011): Delay of the first transition of Asian summer monsoon under global warming condition. SOLA, 7, 81–84.

40) Seiki, A., Y.N. Takayabu, T. Yasuda, N. Sato, C. Takahashi, K. Yoneyama, and R. Shirooka (2011): Westerly wind bursts and their relationship with ENSO in CMIP3 models. J. Geophys. Res., 116, D03303.

41) Takahashi, C., N. Sato, A. Seiki, K. Yoneyama, and R. Shirooka (2011): Projected future change of MJO and its extratropical teleconnection in East Asia during the northern winter simulated in IPCC AR4 models. SOLA, 7, 201–204.

42) Ninomiya, K. (2011): Characteristics of the Meiyu and Baiu frontal precipitation zone in the CMIP3 20th century simulation and 21st century projection. J. Meteor. Soc. Japan, 89, 151–159

43) Kawatani, Y. and K. Ninomiya (2011): The North Pacific subtropical high in August in twentieth-century CMIP3 multimodel dataset. J. Meteor. Soc. Japan, 89, 375–386.

44) Kawatani, Y., K. Hamilton, and S. Watanabe (2011): The Quasi-biennial oscillation in a double CO $ _{2} $ climate. J. Atmos. Sci., 68, 265–283.

45）道広有理，佐藤嘉展，鈴木靖（2011）：CMIP3マルチ気候モデルにおける日本陸域を対象として地上気象要素の再現性・不確実性評価．水文・水資源学会誌，24，5，280-291.

46）道広有理，鈴木靖，佐藤嘉展（2011）：気候変動情報データベースの開発とその利用．土木学会論文集B2（海岸工学），67，2，I_1211-I_1215.

47) Hirota, N. and Y. N. Takayabu (2012): Inter-model differences of future precipitation changes in CMIP3 and MIROC5 climate models. J. Meteor. Soc. Japan, 90A, 307–316. doi:10.2151/jmsj.2012-A16.

48) Nishii, K., T. Miyasaka, H. Nakamura, Y. Kosaka, S. Yokoi, Y. N. Takayabu, H. Endo, H. Ichikawa, T. Inoue, K. Oshima, N. Sato, and Y. Tsushima (2012): Relationship of the reproducibility of multiple variables among global climate models. J. Meteor. Soc. Japan, 90A, 87–100.

49) Wu, L., W. Cai, L. Zhang, H. Nakamura, A. Timmermann, T. Joyce, M. J. McPhaden, M. A. Alexander, B. Qiu, M. Visbeck, P. Chang, and B. Giese (2012): Enhanced warming over the global subtropical western boundary currents. Nature Climate Change, 2, 3, 161–166, doi:10.1038/nclimate1353.

50) Endo, H. (2012): Future changes of Yamase bringing unusually cold summers over northeastern Japan in CMIP3 multi-models. J. Meteor. Soc. Japan, 90A, 123-136.

51) Oshima, K., Y. Tanimoto, and S.-P. Xie (2012): Regional patterns of wintertime SLP change over the North Pacific and their uncertainty in CMIP3 multi-model projections. J. Meteor. Soc. Japan, 90A, 385–396.

52) Takahashi, C., K. Yoneyama, N. Sato, A. Seiki, R. Shirooka, and Y.N. Takayabu (2012): The Madden-Julian Oscillation and extratropical teleconnection over East Asia during the Northern winter in IPCC AR4 climate models, J. Meteor. Soc. Japan, 90A, 361-371.

53) Ninomiya, K. (2012): Year-to-year variations in the Meiyu and Baiu frontal precipitation zone in the CMIP3 20th century simulation. J. Meteor. Soc. Japan, 90A, 317–325.

54) Ninomiya, K. (2012): Characteristics of intense rainfalls over southwestern Japan in the CMIP3 20th century simulation and 21st century projection. J. Meteo. Soc. Japan, 90A, 327–338.

55) Kawatani, Y., K. Hamilton, and A. Noda (2012): The effects of changes in sea surface temperature and CO $ _{2} $ concentration on the quasi-biennial oscillation. J. Atmos. Sci., in press.

56) Ichikawa, H., H. Masunaga, Y. Tsushima, and H. Kanzawa (2012): Reproducibility by climate models of cloud radiative forcing associated with tropical convection. J. Climate, Vol. 25, No. 4, 1247–1262. doi: 10.1175/JCLL-D-11-00114.1.

57) Yara, Y., K. Oshima, M. Fujii, H. Yamano, Y. Yamanaka, and N. Okada (2012): Projection and uncertainty of the poleward range expansion of coral habitats in response to sea surface temperature warming: A multiple climate model study. Galaxea, in press.