[1] Allan, R. P., C. L. Liu, N. G. Loeb, et al., 2014: Changes in global net radiative imbalance 1985–2012. Geophys. Res. Lett., 41, 5588–5597. doi: 10.1002/2014gl060962
[2] Behera, S. K., and T. Yamagata, 2001: Subtropical SST dipole events in the southern Indian Ocean. Geophys. Res. Lett., 28, 327–330. doi: 10.1029/2000GL011451
[3] Cao, J., P. Yao, L. Wang, et al, 2014: Summer rainfall variability in low-latitude highlands of China and subtropical Indian Ocean dipole. J. Climate, 27, 880–892. doi: 10.1175/JCLI-D-13-00121.1
[4] Chambers, D. P., B. D. Tapley, and R. H. Stewart, 1999: Anomalous warming in the Indian Ocean coincident with El Niño. J. Geophys. Res. Oceans, 104, 3035–3047. doi: 10.1029/1998JC900085
[5] Chen, Z. S., Y. Du, Z. P. Wen, et al., 2019: Evolution of south tropical Indian Ocean warming and the climatic impacts following strong El Niño events. J. Climate, 32, 7329–7347. doi: 10.1175/JCLI-D-18-0704.1
[6] Chowdary, J. S., C. Gnanaseelan, and S. P. Xie, 2009: Westward propagation of barrier layer formation in the 2006–07 Rossby wave event over the tropical southwest Indian Ocean. Geophys. Res. Lett., 36, L04607. doi: 10.1029/2008GL036642
[7] Du, Y., and S. P. Xie, 2008: Role of atmospheric adjustments in the tropical Indian Ocean warming during the 20th century in climate models. Geophys. Res. Lett., 35, L08712. doi: 10.1029/2008GL033631
[8] Han, W. Q., J. Vialard, M. J. McPhaden, et al., 2014: Indian Ocean decadal variability: A review. Bull. Amer. Meteor. Soc., 95, 1679–1703. doi: 10.1175/BAMS-D-13-00028.1
[9] Hoerling, M. P., J. W. Hurrell, and T. Y. Xu, 2001: Tropical origins for recent North Atlantic climate change. Science, 292, 90–92. doi: 10.1126/science.1058582
[10] Hu, S. N., and A. V. Fedorov, 2019: Indian Ocean warming can strengthen the Atlantic meridional overturning circulation. Nat. Climate Change, 9, 747–751. doi: 10.1038/s41558-019-0566-x
[11] Huang, B. Y., P. W. Thorne, V. F. Banzon, et al., 2017: Extended reconstructed sea surface temperature, version 5 (ERSSTv5): Upgrades, validations, and intercomparisons. J. Climate, 30, 8179–8205. doi: 10.1175/JCLI-D-16-0836.1
[12] Johnson, E. S., F. Bonjean, G. S. E. Lagerloef, et al., 2007: Validation and error analysis of OSCAR sea surface currents. J. Atmos. Oceanic Technol., 24, 688–701. doi: 10.1175/JTECH1971.1
[13] Kaplan, A., M. A. Cane, Y. Kushnir, et al., 1998: Analyses of global sea surface temperature 1856–1991. J. Geophys. Res. Oceans, 103, 18,567–18,589. doi: 10.1029/97jc01736
[14] Kaufmann, R. K., H. Kauppi, M. L. Mann, et al., 2011: Reconciling anthropogenic climate change with observed temperature 1998–2008. Proc. Natl. Acad. Sci. USA, 108, 11,790–11,793. doi: 10.1073/pnas.1102467108
[15] Lee, S. K., W. Park, M. O. Baringer, et al., 2015: Pacific origin of the abrupt increase in Indian Ocean heat content during the warming hiatus. Nat. Geosci., 8, 445–449. doi: 10.1038/ngeo2438
[16] Li, Y. L., W. Q. Han, and L. Zhang, 2017: Enhanced decadal warming of the southeast Indian Ocean during the recent global surface warming slowdown. Geophys. Res. Lett., 44, 9876–9884. doi: 10.1002/2017GL075050
[17] Liu, W., S. P. Xie, and J. Lu, 2016: Tracking ocean heat uptake during the surface warming hiatus. Nat. Commun., 7, 10926. doi: 10.1038/ncomms10926
[18] Luo, J. J., W. Sasaki, and Y. Masumoto, 2012: Indian Ocean warming modulates Pacific climate change. Proc. Natl. Acad. Sci. USA, 109, 18,701–18,706. doi: 10.1073/pnas.1210239109
[19] Nigam, S., and H. S. Shen, 1993: Structure of oceanic and atmospheric low-frequency variability over the tropical Pacific and Indian oceans. Part I: COADS observations. J. Climate, 6, 657–676. doi: 10.1175/1520-0442(1993)006<0657:sooaal>2.0.co;2
[20] Onogi, K., J. Tsutsui, H. Koide, et al., 2007: The JRA-25 reanaly-sis. J. Meteor. Soc. Japan, 85, 369–432. doi: 10.2151/jmsj.85.369
[21] Rao, S. A., and S. K. Behera, 2005: Subsurface influence on SST in the tropical Indian Ocean: Structure and interannual variability. Dyn. Atmos. Oceans, 39, 103–135. doi: 10.1016/j.dynatmoce.2004.10.014
[22] Rayner, N. A., D. E. Parker, E. B. Horton, et al., 2003: Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J. Geophys. Res. Atmos., 108, 4407. doi: 10.1029/2002JD002670
[23] Reynolds, R. W., and T. M. Smith, 1994: Improved global sea surface temperature analyses using optimum interpolation. J. Climate, 7, 929–948. doi: 10.1175/1520-0442(1994)007<0929:IGSSTA>2.0.CO;2
[24] Roxy, M. K., K. Ritika, P. Terray, et al., 2014: The curious case of Indian Ocean warming. J. Climate, 27, 8501–8509. doi: 10.1175/JCLI-D-14-00471.1
[25] Saha, S., S. Nadiga, C. Thiaw, et al., 2006: The NCEP climate forecast system. J. Climate, 19, 3483–3517. doi: 10.1175/jcli3812.1
[26] Saji, N. H., B. N. Goswami, P. N. Vinayachandran, et al., 1999: A dipole mode in the tropical Indian Ocean. Nature, 401, 360–363. doi: 10.1038/43854
[27] Song, Q., A. L. Gordon, and M. Visbeck, 2004: Spreading of the Indonesian throughflow in the Indian Ocean. J. Phys. Oceanogr., 34, 772–792. doi: 10.1175/1520-0485(2004)034<0772:SOTITI>2.0.CO;2
[28] Su, J. Z., R. H. Zhang, and H. J. Wang, 2017: Consecutive record-breaking high temperatures marked the handover from hiatus to accelerated warming. Sci. Rep., 7, 43735. doi: 10.1038/srep43735
[29] Su, J. Z., R. H. Zhang, T. Li, et al., 2010: Causes of the El Niño and La Niña amplitude asymmetry in the equatorial eastern Pacific. J. Climate, 23, 605–617. doi: 10.1175/2009JCLI2894.1
[30] Tourre, Y. M., and W. B. White, 1995: ENSO signals in global upper-ocean temperature. J. Phys. Oceanogr., 25, 1317–1332. doi: 10.1175/1520-0485(1995)025<1317:ESIGUO>2.0.CO;2
[31] Webster, P. J., A. M. Moore, J. P. Loschnigg, et al., 1999: Coupled ocean–atmosphere dynamics in the Indian Ocean during 1997–98. Nature, 401, 356–360. doi: 10.1038/43848
[32] Wyrtki, K., 1965: Surface currents of the eastern tropical Pacific Ocean. Inter-American Trop. Tuna Comm. Bull., 9, 271–304.
[33] Xie, S. P., H. Annamalai, F. A. Schott, et al., 2002: Structure and mechanisms of South Indian Ocean climate variability. J. Climate, 15, 864–878. doi: 10.1175/1520-0442(2002)015<0864:SAMOSI>2.0.CO;2
[34] Xie, S. P., K. M. Hu, J. Hafner, et al., 2009: Indian Ocean capaci-tor effect on Indo–western Pacific climate during the summer following El Niño. J. Climate, 22, 730–747. doi: 10.1175/2008jcli2544.1
[35] Yamagata, T., S. K. Behera, J. J. Luo, et al., 2004: Coupled ocean–atmosphere variability in the tropical Indian Ocean. Earth’s Climate: The Ocean–Atmosphere Interaction, Volume 147, C. Wang, S. P. Xie, and J. A. Carton, Eds., American Geophysical Union, Washington, D.C., 189–211, doi: 10.1029/147gm12.
[36] Yu, L. S., X. Z. Jin, and R. A. Weller, 2008: Multidecade Global Flux Datasets from the Objectively Analyzed Air–Sea Fluxes (OAFlux) Project: Latent and Sensible Heat Fluxes, Ocean Evaporation, and Related Surface Meteorological Variables. OAFlux Project Technical Report (OA-2008-01), Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, 64 pp.
[37] Zhang, Y., M. Feng, Y. Du, et al., 2018: Strengthened Indonesian throughflow drives decadal warming in the Southern Indian Ocean. Geophys. Res. Lett., 45, 6167–6175. doi: 10.1029/2018GL078265