Response of the Tropical Indian Ocean to Greenhouse Gases and Aerosol Forcing in the GFDL CM3 Coupled Climate Model

References

• Alory, G., & Meyers, G. (2009). Warming of the upper equatorial Indian Ocean and changes in the heat budget (1960–99). Journal of Climate, 22(1), 93–113. doi: 10.1175/2008jcli2330.1
   Web of Science ®Google Scholar
• Bjerknes, J. (1969). Atmospheric teleconnections from the equatorial Pacific. Monthly Weather Review, 97, 163–172. doi: 10.1175/1520-0493(1969)097<0163:ATFTEP>2.3.CO;2
   Web of Science ®Google Scholar
• Boucher, O., Randall, D., Artaxo, P., Bretherton, C., Feingold, G., Forster, P., … Zhang, X. Y. (2013). Clouds and aerosols. In T. F. Stocker, D. Qin, G.-K. Plattner, M. Tignor, S. K. Allen, J. Doschung, A. Nauels, Y. Xia, V. Bex, & P. M. Midgley (Eds.), Climate change 2013: The physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (pp. 571–657). Cambridge: Cambridge University Press. doi: 10.1017/CBO9781107415324.016
   Google Scholar
• Cai, W., & Cowan, T. (2013). Why is the amplitude of the Indian Ocean Dipole overly large in CMIP3 and CMIP5 climate models? Geophysical Research Letters, 40(6), 1200–1205. doi: 10.1002/grl.50208
   Web of Science ®Google Scholar
• Cai, W., Cowan, T., & Raupach, M. (2009). Positive Indian Ocean Dipole events precondition southeast Australia bushfires. Geophysical Research Letters, 36(19), L19710. doi: 10.1029/2009gl039902
   Web of Science ®Google Scholar
• Cai, W., Cowan, T., & Sullivan, A. (2009). Recent unprecedented skewness towards positive Indian Ocean Dipole occurrences and its impact on Australian rainfall. Geophysical Research Letters, 36(11), L11705. doi: 10.1029/2009gl037604
   Google Scholar
• Cai, W. J., Zheng, X. T., Weller, E., Collins, M., Cowan, T., Lengaigne, M., & Yamagata, T. (2013). Projected response of the Indian Ocean Dipole to greenhouse warming. Nature Geoscience, 6, 999–1007. doi: 10.1038/ngeo2009
   Web of Science ®Google Scholar
• Cai, W., & Qiu, Y. (2013). An observation-based assessment of nonlinear feedback processes associated with the Indian Ocean Dipole. Journal of Climate, 26(9), 2880–2890. doi: 10.1175/jcli-d-12-00483.1
   Web of Science ®Google Scholar
• Cai, W., Santoso, A., Wang, G., Weller, E., Wu, L., Ashok, K., … Yamagata, T. (2014). Increased frequency of extreme Indian Ocean Dipole events due to greenhouse warming. Nature, 510(7504), 254–258. doi: 10.1038/nature13327
   PubMed Web of Science ®Google Scholar
• Cai, W., van Rensch, P., Cowan, T., & Hendon, H. H. (2012). An asymmetry in the IOD and ENSO teleconnection pathway and its impact on Australian climate. Journal of Climate, 25(18), 6318–6329. doi: 10.1175/jcli-d-11-00501.1
   Web of Science ®Google Scholar
• Collier, M. A., Rotstayn, L. D., Kim, K.-Y., Hirst, A. C., & Jeffrey, S. J. (2013). Ocean circulation response to anthropogenic aerosol and greenhouse gas forcing in the CSIRO-Mk3.6 coupled climate model. Australian Meteorological and Oceanographic Journal, 63(1), 27–39. doi: 10.22499/2.6301.003
   Google Scholar
• Cowan, T., Cai, W., Ng, B., & England, M. (2015). The response of the Indian Ocean Dipole asymmetry to anthropogenic aerosols and greenhouse gases. Journal of Climate, 28(7), 2564–2583. doi: 10.1175/jcli-d-14-00661.1
   Web of Science ®Google Scholar
• Dong, L., & Zhou, T. (2014). The Indian Ocean sea surface temperature warming simulated by CMIP5 models during the twentieth century: Competing forcing roles of GHGs and anthropogenic aerosols. Journal of Climate, 27(9), 3348–3362. doi: 10.1175/jcli-d-13-00396.1
   Web of Science ®Google Scholar
• Donner, L. J., Wyman, B. L., Hemler, R. S., Horowitz, L. W., Ming, Y., Zhao, M., … Zeng, F. (2011). The dynamical core, physical parameterizations, and basic simulation characteristics of the atmospheric component AM3 of the GFDL global coupled model CM3. Journal of Climate, 24(13), 3484–3519. doi: 10.1175/2011jcli3955.1
   Web of Science ®Google Scholar
• Griffies, S. M., Winton, M., Donner, L. J., Horowitz, L. W., Downes, S. M., Farneti, R., … Zadeh, N. (2011). The GFDL CM3 coupled climate model: Characteristics of the ocean and sea ice simulations. Journal of Climate, 24(13), 3520–3544. doi: 10.1175/2011jcli3964.1
   Web of Science ®Google Scholar
• Hong, C.-C., & Li, T. (2010). Independence of SST skewness from thermocline feedback in the eastern equatorial Indian Ocean. Geophysical Research Letters, 37(11), L11702. doi: 10.1029/2010gl043380
   Google Scholar
• Hong, C.-C., Li, T., Ho, L., & Kug, J.-S. (2008). Asymmetry of the Indian Ocean Dipole. Part I: Observational analysis. Journal of Climate, 21(18), 4834–4848. doi: 10.1175/2008jcli2222.1
   Web of Science ®Google Scholar
• Ihara, C., Kushnir, Y., & Cane, M. A. (2008). Warming trend of the Indian Ocean SST and Indian Ocean Dipole from 1880 to 2004. Journal of Climate, 21(10), 2035–2046. doi: 10.1175/2007jcli1945.1
   Web of Science ®Google Scholar
• Li, T., Wang, B., Chang, C.-P., & Zhang, Y. (2003). A theory for the Indian Ocean Dipole-zonal mode. Journal of the Atmospheric Sciences, 60, 2119–2135. doi: 10.1175/1520-0469(2003)060<2119:ATFTIO>2.0.CO;2
   Web of Science ®Google Scholar
• Liu, F., Luo, Y., Lu, J., Garuba, O., & Wan, X. (2017). Asymmetric response of the equatorial Pacific SST to climate warming and cooling. Journal of Climate, 30(18), 7255–7270. doi: 10.1175/jcli-d-17-0011.1
   Web of Science ®Google Scholar
• Liu, W., Lu, J., & Xie, S.-P. (2015). Understanding the Indian Ocean response to double CO2 forcing in a coupled model. Ocean Dynamics, 65(7), 1037–1046. doi: 10.1007/s10236-015-0854-6
   Web of Science ®Google Scholar
• Luo, Y., Lu, J., Liu, F., & Wan, X. (2016). The positive Indian Ocean Dipole–like response in the tropical Indian Ocean to global warming. Advances in Atmospheric Sciences, 33(4), 476–488. doi: 10.1007/s00376-015-5027-5
   Web of Science ®Google Scholar
• Ng, B., Cai, W., & Walsh, K. (2014). Nonlinear feedbacks associated with the Indian Ocean Dipole and their response to global warming in the GFDL-ESM2M coupled climate model. Journal of Climate, 27(11), 3904–3919. doi: 10.1175/jcli-d-13-00527.1
   Web of Science ®Google Scholar
• Ogata, T., Xie, S.-P., Lan, J., & Zheng, X. (2013). Importance of ocean dynamics for the skewness of the Indian Ocean Dipole mode. Journal of Climate, 26(7), 2145–2159. doi: 10.1175/jcli-d-11-00615.1
   Web of Science ®Google Scholar
• Rotstayn, L. D., Jeffrey, S. J., Collier, M. A., Dravitzki, S. M., Hirst, A. C., Syktus, J. I., & Wong, K. K. (2012). Aerosol- and greenhouse gas-induced changes in summer rainfall and circulation in the Australasian region: A study using single-forcing climate simulations. Atmospheric Chemistry and Physics, 12(14), 6377–6404. doi: 10.5194/acp-12-6377-2012
   Web of Science ®Google Scholar
• Saji, N. H., Goswami, B. N., Vinayachandran, P. N., & Yamagata, T. (1999). A dipole mode in the tropical Indian Ocean. Nature, 401, 360–363. doi: 10.1038/43854
   PubMed Web of Science ®Google Scholar
• Song, Q., Vecchi, G. A., & Rosati, A. J. (2007). The role of the Indonesian throughflow in the Indo–Pacific climate variability in the GFDL coupled climate model. Journal of Climate, 20(11), 2434–2451. doi: 10.1175/jcli4133.1
   Web of Science ®Google Scholar
• Sprintall, J., Wijffels, S. E., Molcard, R., & Jaya, I. (2009). Direct estimates of the Indonesian throughflow entering the Indian Ocean: 2004–2006. Journal of Geophysical Research, 114(C7), 114, C07001. doi: 10.1029/2008jc005257
   Web of Science ®Google Scholar
• Taylor, K. E., Stouffer, R. J., & Meehl, G. A. (2012). An overview of CMIP5 and the experiment design. Bulletin of the American Meteorological Society, 93(4), 485–498. doi: 10.1175/bams-d-11-00094.1
   Web of Science ®Google Scholar
• Wallace, J. M., & Hobbs, P. V. (2006). Atmospheric science: An introductory survey (2nd ed.). Salt Lake City, USA: Academic Press.
   Google Scholar
• Wang, H., Xie, S.-P., & Liu, Q. (2016). Comparison of climate response to anthropogenic aerosol versus greenhouse gas forcing: Distinct patterns. Journal of Climate, 29(14), 5175–5188. doi: 10.1175/jcli-d-16-0106.1
   Web of Science ®Google Scholar
• Weller, E., & Cai, W. (2013). Realism of the Indian Ocean Dipole in CMIP5 models: The implications for climate projections. Journal of Climate, 26(17), 6649–6659. doi: 10.1175/jcli-d-12-00807.1
   Web of Science ®Google Scholar
• Xie, S.-P., Deser, C., Vecchi, G. A., Ma, J., Teng, H., & Wittenberg, A. T. (2010). Global warming pattern formation: Sea surface temperature and rainfall. Journal of Climate, 23(4), 966–986. doi: 10.1175/2009jcli3329.1
   Web of Science ®Google Scholar
• Xie, S.-P., Lu, B., & Xiang, B. (2013). Similar spatial patterns of climate responses to aerosol and greenhouse gas changes. Nature Geoscience, 6, 828–832. doi: 10.1038/NGEO1931
   Web of Science ®Google Scholar
• Zheng, X.-T., Xie, S.-P., Du, Y., Liu, L., Huang, G., & Liu, Q. (2013). Indian Ocean Dipole response to global warming in the CMIP5 multimodel ensemble. Journal of Climate, 26(16), 6067–6080. doi: 10.1175/jcli-d-12-00638.1
   Web of Science ®Google Scholar
• Zheng, X.-T., Xie, S.-P., Vecchi, G. A., Liu, Q., & Hafner, J. (2010). Indian Ocean Dipole response to global warming: Analysis of ocean–atmospheric feedbacks in a coupled model. Journal of Climate, 23(5), 1240–1253. doi: 10.1175/2009jcli3326.1
   Web of Science ®Google Scholar