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张亚洲
2023-05-16 12:28
  • 张亚洲
  • 张亚洲 - 博士 讲师-中国海洋大学-海洋与大气学院-个人资料

近期热点

资料介绍

个人简历


教育经历:
2011/09-2015/06 西北师范大学地理科学学士
2015/09-2020/06 北京师范大学全球环境变化博士

工作经历:
2020/09-至今中国海洋大学海洋与大气学院讲师

主要项目:
[1] 2017/06-2018/05,北京师范大学青年人才项目,主持
[2] 2017/01-2021/06,海洋局国际合作项目太平洋-印度洋与亚洲季风的相互影响(主持:李建平教授),参与
[3] 2016-2020,国家自然科学重点基金扰动位能在东亚夏季风变化中的作用及其可预报性(主持:李建平教授),参与

研究领域


季风动力学、海气相互作用、大气能量学""

近期论文


[1] Zhang, Y. Z., J. P. Li*, S. Zhao, F. Zheng, J. Feng, Y. Li and Y. D. Xu, 2020: Indian Ocean tripole mode and its associated atmospheric and oceanic processes. Climate Dynamics, 55:1367–1383, https://doi.org/10.1007/s00382-020-05331-1.
[2] Zhang Y. Z., J. P. Li*, J. Q. Xue, F. Zheng, R. G. Wu, K. J. Ha, and J. Feng, 2019: The relative roles of the South China Sea summer monsoon and ENSO in the Indian Ocean dipole development. Climate Dynamics, 53(11), 6665-6680, https://doi.org/10.1007/s00382-019-04953-4.
[3] Zhang Y. Z., J. P. Li*, Q.Y. Wang, and J. Q. Xue, 2019: Variations in the atmospheric perturbation potential energy associated with the South China Sea summer monsoon. Climate Dynamics, 53(3-4), 2295-2308, https://doi.org/10.1007/s00382-019-04845-7.
[4] Zhang Y. Z., J. P. Li*, J. Q. Xue, J. Feng, Q. Y. Wang, Y. D. Xu, and Y. H. Wang, 2018: Impact of the South China Sea summer monsoon on the Indian Ocean dipole. Journal of Climate, 31(16), 6557-6572, https://doi.org/10.1175/JCLI-D-17-0815.1.
[5] Wang Y. H., J. P. Li*, Y. Z. Zhang, Q. Y. Wang, J. H. Qin, 2019: Atmospheric energetics over the tropical Indian Ocean during Indian Ocean dipole events. Climate Dynamics, 52(9-10), 6243-6256,https://doi.org/10.1007/s00382-018-4510-y.
[6] Sun R. N., J. P. Li, J. Feng, Z. L. Hou, and Y. Z. Zhang, Contrasting impacts of two types of El Niño on the yields of early rice in Southern China. Agronomy Journal, 112(2), 2020, 1084-1100, https://doi.org/10.1002/agj2.20014.
[7] Wang, Q. Y., J. P. Li, Y. J. Li, J. Q. Xue, S. Zhao, Y. D. Xu, Y. H. Wang, Y. Z. Zhang, D. Dong and J. W. Zhang, Modulation of tropical cyclone tracks over the western North Pacific by intra-seasonal Indo-western Pacific convection oscillation during the boreal extended summer. Climate Dynamics, 52(1-2), 2018, 913-927, https://doi.org/10.1007/s00382-018-4264-6.
[8] Xu, Y. D., J. P. Li, C. Sun, X. P. Lin, H. L. Liu, L. N. Wang, Y. S. Liang, Q. Y. Wang, Y. Z. Zhang, Z. L. Hou, and F. C. Wang, Contribution of SST change to multi-decadal global and continental surface air temperature trends between 1910 and 2013. Climate Dynamics, 54(3-4), 2019, 1295–1313, https://doi.org/10.1007/s00382-019-05060-0.

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