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Claire L. Vincent and Todd P. Lane

.1175/1520-0493(1981)109<1595:WMCITV>2.0.CO;2 Huffman , G. J. , and Coauthors , 2007 : The TRMM Multisatellite Precipitation Analysis (TMPA): Quasi-global, multiyear, combined-sensor precipitation estimates at fine scales . J. Hydrometeor. , 8 , 38 – 55 , https://doi.org/10.1175/JHM560.1 . 10.1175/JHM560.1 Jakob , C. , and C. Schumacher , 2008 : Precipitation and latent heating characteristics of the major tropical western Pacific cloud regimes . J. Climate , 21 , 4348 – 4364 , https://doi.org/10.1175/2008JCLI

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Casey D. Burleyson, Samson M. Hagos, Zhe Feng, Brandon W. J. Kerns, and Daehyun Kim

: Diurnal precipitation regimes in the global tropics . J. Climate , 21 , 2680 – 2696 , https://doi.org/10.1175/2007JCLI2051.1 . 10.1175/2007JCLI2051.1 Kiladis , G. N. , J. Dias , K. H. Straub , M. C. Wheeler , S. N. Tulich , K. Kikuchi , K.M. Weickmann , and M. J. Ventrice , 2014 : A comparison of OLR and circulation-based indices for tracking the MJO . Mon. Wea. Rev. , 142 , 1697 – 1715 , https://doi.org/10.1175/MWR-D-13-00301.1 . 10.1175/MWR-D-13-00301.1 Kim , D

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Andung Bayu Sekaranom and Hirohiko Masunaga

.1080/01431161.2013.826837 . 10.1080/01431161.2013.826837 Berg , W. , T. L’Ecuyer , and C. Kummerow , 2006 : Rainfall climate regimes: The relationship of regional TRMM rainfall biases to the environment . J. Appl. Meteor. Climatol. , 45 , 434 – 454 , doi: 10.1175/JAM2331.1 . 10.1175/JAM2331.1 Chang , C.-P. , Z. Wang , J. McBride , and C.-H. Liu , 2005 : Annual cycle of Southeast Asia–Maritime Continent rainfall and the asymmetric monsoon transition . J. Climate , 18 , 287 – 301 , doi: 10.1175/JCLI

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Casey R. Densmore, Elizabeth R. Sanabia, and Bradford S. Barrett

://doi.org/10.1175/MWR-D-13-00301.1 . 10.1175/MWR-D-13-00301.1 Kousky , V. E. , and R. W. Higgins , 2007 : An alert classification system for monitoring and assessing the ENSO cycle . Wea. Forecasting , 22 , 353 – 371 , https://doi.org/10.1175/WAF987.1 . 10.1175/WAF987.1 LaFleur , D. M. , B. S. Barrett , and G. R. Henderson , 2015 : Some climatological aspects of the Madden–Julian oscillation (MJO) . J. Climate , 28 , 6039 – 6053 , https://doi.org/10.1175/JCLI-D-14-00744.1 . 10

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Chen Li, Jing-Jia Luo, and Shuanglin Li

index (5°S–5°N, 160°E–150°W). Namely, the EP (CP) of ENSO event is identified if the magnitude of the Niño-3 index is greater (lower) than that of the Niño-4 index; meanwhile, the magnitude of the Niño-3 (Niño-4) index should be greater than 0.5°C. This classification of the EP and CP types of ENSO follows the method used in Yeh et al. (2009) and Kug et al. (2009) , except that they applied it to DJF (i.e., ENSO peak phase) while the present study focuses on JJA (i.e., ENSO onset/decay phase

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