Impact of different types of La Niña development on the precipitation in the Maritime Continent

References

• Chang, C. P., Li, T., & Yang, S. (2020). Seasonal prediction of boreal winter rainfall over the western maritime continent during ENSO. Journal of Meteorological Research, 34(2), 294–303. https://doi.org/10.1007/s13351-020-9181-z
   Web of Science ®Google Scholar
• Chang, C. P., Wang, Z., Ju, J., & Li, T. (2004). On the relationship between western maritime continent monsoon rainfall and ENSO during northern winter. Journal of Climate, 17(3), 665–672. https://doi.org/10.1175/1520-0442(2004)017<0665:OTRBWM>2.0.CO;2
   Web of Science ®Google Scholar
• Chen, L., & Li, G. (2022). Interdecadal change in the relationship between El Niño in the decaying stage and the central China summer precipitation. Climate Dynamics, 59(7–8), 1981–1996. https://doi.org/10.1007/s00382-022-06192-6
   Web of Science ®Google Scholar
• Chen, L., Li, G., Lu, B., Li, Y. P., Gao, C. J., Long, S. M., Li, X. Y., & Wang, Z. Q. (2022). Two approaches of the spring North Atlantic sea surface temperature affecting the following July precipitation over Central China:the tropical and extratropical Pathways. Journal of Climate, 35(20), 2969–2986. https://doi.org/10.1175/JCLI-D-21-1012.1
   Web of Science ®Google Scholar
• Chen, M., Li, T., Shen, X., & Wu, B. (2016). Relative roles of dynamic and thermodynamic processes in causing evolution asymmetry between El Niño and La Niña. Journal of Climate, 29(6), 2201–2220. https://doi.org/10.1175/JCLI-D-15-0547.1
   Web of Science ®Google Scholar
• Chen, W., & Guan, Z. Y. (2017). A joint monsoon index for East Asian–Australian monsoons during boreal summer. Atmospheric Science Letters, 18(10), 403–408. https://doi.org/10.1002/asl.782
   Web of Science ®Google Scholar
• Chen, W., Guan, Z. Y., Xu, Q., & Yang, H. D. (2019). Variation of anomalous convergence around Kalimantan Island in lower troposphere and its role in connecting the East Asian summer monsoon and Australian winter monsoon. Journal of Geophysical Research-Atmospheres, 124(13), 6892–6903. https://doi.org/10.1029/2018JD030215
   Web of Science ®Google Scholar
• Chen, W., Park, J. K., Dong, B. W., Lu, R. Y., & Jung, W. S. (2012). The relationship between El Niño and the western North Pacific summer climate in a coupled GCM: Role of the transition of El Niño decaying phases. Journal of Geophysical Research-Atmospheres, 117. https://doi.org/10.1029/2011JD017385
   Web of Science ®Google Scholar
• Danabasoglu, G., Lamarque, J. F., Bacmeister, J., Bailey, D. A., DuVivier, A. K., Edwards, J., Emmons, L. K., Fasullo, J., Garcia, R., Gettelman, A., Hannay, C., Holland, M. M., Large, W. G., Lauritzen, P. H., Lawrence, D. M., Lenaerts, J. T. M., Lindsay, K., Lipscomb, W. H., Mills, M. J., … Strand, W. G. (2020). The Community earth system model version 2(CESM2). Journal of Advances in Modeling Earth Systems, 12(2). https://doi.org/10.1029/2019MS001916
   Web of Science ®Google Scholar
• Gao, C. J., & Li, G. (2023). Asymmetric effect of ENSO on the maritime continent precipitation in decaying summers. Climate Dynamics, 61(5–6), 2839–2852. https://doi.org/10.1007/s00382-023-06716-8
   Web of Science ®Google Scholar
• Haylock, M., & McBride, J. (2001). Spatial coherence and predictability of Indonesian Wet Season Rainfall. Journal of Climate, 14(18), 3882–3887. https://doi.org/10.1175/1520-0442(2001)014<3882:scapoi>2.0.co;2
   Web of Science ®Google Scholar
• Hendon, H. H. (2003). Indonesian rainfall variability:impacts of ENSO and local air–sea interaction. Journal of Climate, 16(11), 1775–1790. https://doi.org/10.1175/1520-0442(2003)016<1775:IRVIOE>2.0.CO;2
   Web of Science ®Google Scholar
• Hou, M. Y., & Tang, Y. M. (2022). Recent progress in simulating two types of ENSO - from CMIP5 to CMIP6. Frontiers in Marine Science, 9. https://doi.org/10.3389/fmars.2022.986780
   PubMed Web of Science ®Google Scholar
• Jiang, L. S., & Li, T. (2018). Why rainfall response to El Niño over maritime continent is weaker and non-uniform in boreal winter than in boreal summer. Climate Dynamics, 51(4), 1465–1483. https://doi.org/10.1007/s00382-017-3965-6
   Web of Science ®Google Scholar
• Jiang, W. P., Huang, G., Huang, P., Wu, R. G., Hu, K. M., & Chen, W. (2019). Northwest pacific anticyclonic anomalies during post–El Niño summers determined by the pace of El Niño Decay. Journal of Climate, 32(12), 3487–3503. https://doi.org/10.1175/JCLI-D-18-0793.1
   Web of Science ®Google Scholar
• Li, G., Chen, L., & Lu, B. (2023). A Physics-Based Empirical Model for the Seasonal Prediction of the Central China July Precipitation. Geophysical Research Letters, 50(3), e2022GL101463. https://doi.org/10.1029/2022GL101463
   Google Scholar
• Liu, C. T., & Zipser, E. J. (2005). Global distribution of convection penetrating the tropical tropopause. Journal of Geophysical Research-Atmospheres, 110(D23). https://doi.org/10.1029/2005JD006063
   Web of Science ®Google Scholar
• Neale, R., & Slingo, J. (2003). The maritime continent and its role in the global climate: A GCM study. Journal of Climate, 16(5), 834–848. https://doi.org/10.1175/1520-0442(2003)016<0834:TMCAIR>2.0.CO;2
   Web of Science ®Google Scholar
• Ogino, S. Y., Yamanaka, M. D., Mori, S., & Matsumoto, J. (2016). How much is the precipitation amount over the tropical coastal region? Journal of Climate, 29(3), 1231–1236. https://doi.org/10.1175/JCLI-D-15-0484.1
   Web of Science ®Google Scholar
• Okumura, Y. M., & Deser, C. (2010). Asymmetry in the duration of El Niño and La Niña. Journal of Climate, 23(21), 5826–5843. https://doi.org/10.1175/2010JCLI3592.1
   Web of Science ®Google Scholar
• Philander, S. G. (1983). El Niño/Southern Oscillation phenomena. Nature, 302(5906), 295–301. https://doi.org/10.1038/302295a0
   Web of Science ®Google Scholar
• Ramage, C. S. (1968). Role of a tropical “Maritime Continent” in the atmospheric circulation. Monthly Weather Review, 96(6), 365–370. https://doi.org/10.1175/1520-0493(1968)096<0365:roatmc>2.0.co;2
   Web of Science ®Google Scholar
• Ropelewski, C. F., & Halpert, M. S. (1987). Global and regional scale precipitation patterns associated with the El Niño/Southern Oscillation. Monthly Weather Review, 115(8), 1606–1626. https://doi.org/10.1175/1520-0493(1987)115<1606:GARSPP>2.0.CO;2
   Web of Science ®Google Scholar
• Ropelewski, C. F., & Halpert, M. S. (1989). Precipitation patterns associated with the high index phase of the Southern Oscillation. Journal of Climate, 2(3), 268–284. https://doi.org/10.1175/1520-0442(1989)002<0268:PPAWTH>2.0.CO;2
   Web of Science ®Google Scholar
• Simpson, J., Keenan, T. D., Ferrier, B., Simpson, R. H., & Holland, G. J. (1993). Cumulus mergers in the maritime continent region. Meteorology and Atmospheric Physics, 51(1–2), 73–99. https://doi.org/10.1007/BF01080881
   Web of Science ®Google Scholar
• Song, D. W., Guan, Z. Y., & Tang, W. Y. (2011). Variations of OLR in Maritime Continent Regions in association with droughts and floods in the upper and middle reaches of Yangtze River of China in boreal summer [in Chinese]. Journal of Tropical Meteorology, 27(4), 560–568. https://doi.org/10.3969/j.issn.1004-4965.2011.04.013
   Google Scholar
• Timmermann, A., An, S. I., Kug, J. S., Jin, F. F., Cai, W. J., Capotondi, A., Cobb, K. M., Lengaigne, M., McPhaden, M. J., Stuecker, M. F., Stein, K., Wittenberg, A. T., Yun, K.-S., Bayr, T., Chen, H.-C., Chikamoto, Y., Dewitte, B., Dommenget, D., Grothe, P., … Zhang, X. B. (2018). El Niño-Southern Oscillation complexity. Nature, 559(7715), 535–545. https://doi.org/10.1038/s41586-018-0252-6
   PubMed Web of Science ®Google Scholar
• Wang, W. T., & Guan, Z. Y. (2018). The SSTA patterns of El Niño-Modoki and eastern Pacific ENSO and their associations with regional climate variation in the Maritime Continent during boreal summer [in Chinese]. Acta Meteorologica Sinica, 76(1), 1–14. https://doi.org/10.11676/qxxb2017.081
   Google Scholar
• Wu, X. B., Li, G., Jiang, W. P., Long, S. M., & Lu, B. (2021). Asymmetric relationship between ENSO and the tropical Indian Ocean summer SST anomalies. Journal of Climate, 34(14), 5955–5969. https://doi.org/10.1175/JCLI-D-20-0546.1
   Web of Science ®Google Scholar
• Xu, Q., & Guan, Z. Y. (2017). Interannual variability of summertime outgoing longwave radiation over the Maritime Continent in relation to East Asian summer monsoon anomalies. Journal of Meteorological Research, 31(4), 665–677. https://doi.org/10.1007/s13351-017-6178-3
   Web of Science ®Google Scholar
• Yang, S., Zhang, T. T., Li, Z. N., & Dong, S. R. (2019). Climate variability over the maritime continent and its role in global climate variation: A review. Journal of Meteorological Research, 33(6), 993–1015. https://doi.org/10.1007/s13351-019-9025-x
   Web of Science ®Google Scholar
• Yang, X. K., & Huang, P. (2021). Restored relationship between ENSO and Indian summer monsoon rainfall around 1999/2000. Innovation, 2, 100102. https://doi.org/10.1016/j.xinn.2021.100102
   Google Scholar
• Yang, X. K., Huang, P., Hu, P., & Wang, Z. B. (2023). Distinct impacts of two types of summer ENSO with different temporal evolutions on the Asian Summer Monsoon: Role of the Tropical Indo-western Pacific. Journal of Climate, 36(12), 3917–3936. https://doi.org/10.1175/JCLI-D-22-0532.1
   Web of Science ®Google Scholar
• Yang, X. K., Huang, P., Liu, Y., & Chen, D. (2022). An interdecadal enhancement of the impact of ENSO on the summer Northeast Asia circulation around 1999/2000 through the Silk Road Pattern. Journal of Climate, 35(22), 3881–3897. https://doi.org/10.1175/JCLI-D-22-0195.1
   Web of Science ®Google Scholar