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Yuta Ando, Masayo Ogi, and Yoshihiro Tachibana

air did not reach the surface of the earth in October (during P1), however, in spite of the strong negative AO and WP values then. Anomalous positive sensible and latent heat fluxes during P1 and P2 indicate that heat from the ocean was released to the atmosphere during these periods ( Fig. 1e ). The negative AO and WP, which tended to cool SATs around Japan, also led to these positive heat fluxes. During October, the record-breaking warm SST (normalized interannual SST index was +1.72) offset the

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Ayumu Miyamoto, Hisashi Nakamura, and Takafumi Miyasaka

– 3401 , https://doi.org/10.1175/2010JCLI3910.1 . 10.1175/2010JCLI3910.1 Hubanks , P. , S. Platnick , M. King , and B. Ridgway , 2016 : MODIS Atmosphere L3 Gridded Product Algorithm Theoretical Basis Document (ATBD) and Users Guide. NASA GSFC, MODIS Tech. Doc. ATBD-MOD-30, 122 pp., https://modis-images.gsfc.nasa.gov/_docs/L3_ATBD_C6.pdf . Hwang , Y.-T. , and D. M. W. Frierson , 2013 : Link between the double-Intertropical Convergence Zone problem and cloud biases over the Southern

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