米兰milan官方网站



彭启华

副教授、至诚青年教授


邮箱: qpeng@nju.edu.cn
个人主页: https://qihuapengclimate.github.io/

工作经历概述

彭启华,米兰milan官方网站副教授,至诚青年教授,博士生导师,国家级青年人才计划入选者。研究领域主要包括海气相互作用、海洋动力学和气候变化,专注于厄尔尼诺-南方涛动新动力机制的探索以及全球变暖对海洋和大气系统的影响。以第一作者在Nature Climate Change、Nature Geoscience、Nature Communications、Science Advances等国际顶级期刊发表多篇研究论文。成果入选 ESI 热点论文与高被引论文,获Science、NASA、CBS、NPR 等国际权威媒体专题报道。研究成果入选“中国海洋与湖沼十大科技进展”以及中国科学院“优秀博士学位论文”(全国每年100篇)。合作出版学术专著1部。担任Nature、Nature Climate Change、Nature Communications、Science Advances、Journal of Climate、Geophysical Research Letters等国际知名期刊审稿人。

目前课题组诚招博士后、博士生及硕士生,有意者欢迎发送邮件至qpeng@nju.edu.cn与我联系。

教育背景
 2013 - 2019中国科学院南海海洋研究所,物理海洋学博士
 2016 - 2018加州大学圣地亚哥分校斯克里普斯海洋研究所,物理海洋学联合培养博士
 2009 - 2013南京大学,海洋科学学士
工作经历
 2026 - 至今米兰milan官方网站,副教授、至诚青年教授
 2021 - 2025加州大学圣地亚哥分校斯克里普斯海洋研究所,博士后研究员
 2019 - 2021中国科学院南海海洋研究所,助理研究员
研究兴趣

海气相互作用;厄尔尼诺-南方涛动(ENSO);气候变化;海洋动力学

发表的论文
Peng, Q., Xie, S. P., Miyamoto, A., Deser, C., Zhang, P., & Luongo, M. T. (2025). Strong 2023–2024 El Niño generated by ocean dynamics. Nature Geoscience, 1-8.
Peng, Q., Xie, S.-P., & Deser, C., (2024). Collapsed upwelling weakens ENSO under sustained warming beyond the 21st century. Nature Climate Change, 14(8), 815-822.
Peng, Q., Xie, S.-P., Passalacqua, G., Miyamoto A., & Deser, C., (2024). The 2023 extreme coastal El Niño: Atmospheric and air-sea coupling mechanisms. Science Advances, 10(12).
Peng, Q., Xie, S.-P., Huang R., Wang, W., Zu, T., & Wang, D. (2023). Indonesian Throughflow slowdown under global warming: Remote AMOC effect vs. regional surface forcing. Journal of Climate, 36(5),1301-1318.
Peng, Q., Xie, S.-P., Wang, D., Huang R., Chen G., Shu Y., et al. (2022). Surface warming–induced global acceleration of upper ocean currents. Science Advances, 8(16).
Peng, Q., Xie, S.-P., Wang, D., Kamae, Y., Zhang, H., Hu, S., et al. (2020). Eastern Pacific wind effect on the evolution of El Niño: Implications for ENSO diversity. Journal of Climate, 33(8), 3197-3212.
Peng, Q., Xie, S.-P., Wang, D., Zheng, X.-T., & Zhang, H. (2019). Coupled ocean-atmosphere dynamics of the 2017 extreme coastal El Niño. Nature Communications, 10(1), 298.
Xie, S.-P., Peng, Q.#(co-first author), Kamae, Y., Zheng, X.-T., Tokinaga, H., & Wang, D. (2018). Eastern Pacific ITCZ dipole and ENSO diversity. Journal of Climate, 31(11), 4449-4462.
Peng, Q., Huang, R.-X., Wang, W., & Wang, D. (2020). The main heaving modes in the Pacific Ocean. Journal of Tropical Oceanography, 39(2), 1-10.
Zheng, X., Long, S., Zhou Z.Q., Peng, Q., Wang C. (Trans.) (2025). Coupled Atmosphere-Ocean Dynamics: From El Niño to Climate Change (Chinese Edition). Science Press.
Chen, T., Wang, D., Huang, K. and Peng, Q., 2025. Distinct phase-locked local and remote forcing deepens the summer thermocline in the Southern Bay of Bengal. Ocean Dynamics, 75(11), 95.
Ren Q., Xie, S. P., Peng, Q., Li Y., & Wang F. (2025). Equatorial Atlantic mid-depth warming indicates Atlantic meridional overturning circulation slowdown. Communications Earth & Environment, 6, 819.
Cheng, L., ... Peng, Q., ... & Yuan, H. (2025). Ocean stratification in a warming climate. Nature Reviews Earth & Environment, 1-19.
Shu, Y., Lu, X., Xia, R., Peng, Q., & Wang, D. (2025). Heaving induced by PDO driving abyssal water decadal variability in the Eastern Philippine Sea. Geophysical Research Letters, 52(19), e2025GL116364.
Taylor, B. A., Shi, J. R., Xie, S. P., Talley, L. D., Luongo, M. T., & Peng, Q. (2025). Warming Band in Southern Ocean’s Indian Sector: The Role of Remote Atlantic Buoyancy Forcing via Poleward-Shifting Circulation Response. Journal of Climate, 38(14), 3219-3238.
Luongo, M. T., Xie, S. P., Eisenman, I., Sun, S., & Peng, Q. (2025). How the Subsurface Tropical Pacific Responds to Subtropical Surface Cooling: Implications for Cross-Equatorial Transport. Journal of Climate.
Luo, X., Yang, L., Chan, J.C., Chen, S., Peng, Q., & Wang, D., (2024). China coasts facing more tropical cyclone risks during the second decaying summer of double-year La Niña events. npj Climate and Atmospheric Science, 7(1), 198.
Zhou, X., Zhou, W., Wang, D., Xie, Q., Yang, L. and Peng, Q., (2024). Westerlies Affecting the Seasonal Variation of Water Vapor Transport over the Tibetan Plateau Induced by Tropical Cyclones in the Bay of Bengal. Advances in Atmospheric Sciences, 41(5), 881-893.
Wang, S., Jing, Z., Wu, L., Sun, S., Peng, Q., Wang, H., et al. (2023). Southern hemisphere eastern boundary upwelling systems emerging as future marine heatwave hotspots under greenhouse warming. Nature Communications, 14(1), 28.
Li, Y., Xie, S.P., Lian, T., Zhang, G., Feng, J., Ma, J., Peng, Q., Wang, W., Hou, Y. and Li, X., (2023). Interannual variability of regional Hadley circulation and El Niño interaction. Geophysical Research Letters, 50(4), e2022GL102016.
Chu, X., & Peng, Q. (2023). The role of alongshore wind and ocean wave in generating the northward Somali Current. Journal of Tropical Oceanography, 42(2), 1-8.
Chen, G., Huang, R. X., Peng, Q., & Chu, X. (2022). A time-dependent Sverdrup relation and its application to the Indian Ocean. Journal of Physical Oceanography, 52(6), 1233-1244.
Liang, Z., Zeng, L., Wang, Q., Peng, Q., & Wang, D. (2022). Interpretation of interannual variability of the zonal contrasting thermal conditions in the winter South China Sea. Climate Dynamics, 1-19.
Zhang, Y., Yu, S.-Y., Xie, S.-P., Amaya, D. J., Peng, Q., Kosaka, Y., et al. (2022). Role of ocean dynamics in equatorial Pacific decadal variability. Climate Dynamics, 59(7-8), 2517-2529.
Zhong, Q., Chen, G., Li, Y., Peng, Q., & Chu, X. (2022). Intraseasonal variability of the surface zonal current in the equatorial Indian Ocean: Seasonal differences and causes. Acta Oceanologica Sinica, 41(5), 12-26.
Shi, J.-R., Talley, L. D., Xie, S.-P., Peng, Q., & Liu, W. (2021). Ocean warming and accelerating Southern Ocean zonal flow. Nature Climate Change.
Zeng, L., Chen, G., Huang, K., Chen, J., He, Y., Zhou, F., Yang, Y., Liang, Z., Peng, Q., Shi, R. and Gamage, T.P., (2021). A decade of eastern tropical Indian Ocean Observation Network (TIOON). Bulletin of the American Meteorological Society, 102(10), E2034-E2052.



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