李元龙，研究员，博士，博士生导师，1983年生。专业为物理海洋学。2012年获物理海洋学博士学位；2017年入选“QR计划”青年项目；2019年获得山东省自然科学一等奖（排名第二）。在JPO、JC、GRL、JGR、NREE等物理海洋学权威期刊共发表论文90多篇，其中第一/通讯作者论文40多篇。近年来主要从事印度洋海洋环流与气候变化方向的研究，聚焦印度洋的年代际和季节内温盐变异，在变异特征、物理机制和气候效应等方面取得了一系列成果。2023年起任国际知名期刊《JGR-Oceans》编委。

一、研究领域  

1. 海洋热力学过程及其气候环境影响

2. 海洋水团与气候变化

二、招生专业及方向专业：物理海洋学

方向：海洋环流与气候环境效应

三、研究室及联系方式       

研究室：海洋环流与波动重点实验室

邮箱：liyuanlong@qdio.ac.cn

办公电话：82893903

四、承担的主要科研项目

1.科技部重点研发专项课题：三大洋相互作用的“海洋通道”过程机制，2019-2024

2.崂山实验室科技创新项目课题: 海-气系统年代际变化规律与机理，2022-2025

3.中国科学院战略性先导科技专项（B类）子课题：东印度洋与印尼海物质能量交换过程，2020-2024

4.山东省杰出青年基金项目：印度洋温盐变化，2021-2023

5.国家自然科学基金面上项目：东南印度洋海温长期变化及其对“海洋热浪”事件的影响，2018-2021

6.中科院海洋大科学研究中心重点部署项目：印度洋中层水团长期变化：物理海洋与古气候学联合研究，2019-2022，在研，主持

7.国家QR计划青年项目：环境与地球科学, 2018-2021，在研，主持

8.国家自然科学基金青年项目：副热带东南印度洋年代变异及其气候效应，2019-2021，24万元，在研，主持         

五、研究成果及奖励         

主要研究成果包括：1）揭示了印度洋热含量的年代际振荡特征及其三维结构，指明了印尼贯穿流的重要作用，系统阐释了其振荡机理;2）发现了东南印度洋的热量集聚现象，指出了其对“海洋热浪”和澳洲洪涝灾害的促进作用；3）探明了调控热带印度洋海温和盐度季节内变异的关键过程，提出了南亚季风季节内振荡的海气耦合理论模型；4）发现了孟加拉湾盐度对南亚季风季节内振荡的影响，阐释了盐度通过改变海洋层结影响季风变异事件发展的完整过程。

主要奖励：

六、代表性论文及著作

（*代表通讯作者）

⁃ Wang, F.*, Li, X., Tang, X., Sun, X., Zhang, J., Yang, D., Xu, L., Zhang, H., Wang, Y., Yao, Y., Wang, C., Guo, Y., Ren, Q., Li, Y.*, Zhang, R., Wang, X., Zhang, B., Sha, Z., 2023, The seas around China in a warming climate, Nature Review Earth & Environment, 4, 535–551. DOI: 10.1038/s43017-023-00453-6

⁃ Guo, Y., Li, Y.*, Cheng, Li., Chen, G., Liu, Q.-Y., Tian, T., Hu, S., Wang, J., Wang, F., 2023: An updated estimate of the Indonesian Throughflow geostrophic transport: inter-annual variability and salinity effect, Geophysical Research Letters, 50, e2023GL103748. 
 

⁃ Guo, Y., Li, Y.*, Wang, F., 2023: Destinations and pathways of the Indonesian Throughflow water in the Indian Ocean, Journal of Climate, 36(11), 3717–3735, https://doi.org/10.1175/JCLI-D-22-0631.1

⁃ Gao, X., Li, Y.*, Lin, P., Zhang, L., Ren, Q., Lu, Y., Wang, F., 2023: Origins of Multidecadal SST Variations in the Southern Atlantic and Indian Oceans since the 1960s, Geophysical Research Letters, 50, e2022GL101735,

⁃ Duan, J., Li, Y.*, Cheng, L., Lin, P., Wang, F. 2023: Heat Storage in the Upper Indian Ocean: the Role of Wind-Driven Redistribution. Journal of Climate, 36(7), 2221-2242.

⁃ Li, J., Li, Y.*, Guo, Y., Li., G., Wang, F. 2023: Decadal variability of sea surface salinity in the southeastern Indian Ocean: roles of local rainfall and the Indonesian throughflow, Frontiers in Marine Science, 9:1097634, doi:10.3389/fmars.2022.1097634

⁃ Li, Y.*, Guo, Y., Zhu, Y., Kido, S., Zhang, L., & Wang, F., 2022: Variability of Heat Content and Eddy Kinetic Energy in the Southeast Indian Ocean: Roles of the Indonesian Throughflow and Local Wind Forcing. Journal of Physical Oceanography, 52(11), 2789-2806.

⁃ Lu, Y., Li, Y.*, Duan, J., Lin, P., & Wang, F., 2022: Multidecadal Sea-level Rise in the Southeast Indian Ocean: The Role of Ocean Salinity Change. Journal of Climate, 35(5), 1479-1496, doi:10.1175/JCLI-D-21-0288.1

⁃ Liu, L.-L., Li, Y.*, & Wang, F. 2022: Reduction of Equatorial Obduction by Atmospheric Intraseasonal Oscillations in the Western and Central Pacific Ocean,  Journal of Geophysical Research Oceans, 127, e2021JC017901,

⁃ Lv, M., Wang, F.*, Li, Y.*, Zhang, Z., & Zhu, Y., 2022: Structure of Sea Surface Temperature Anomaly Induced by Mesoscale Eddies in the North Pacific Ocean, Journal of Geophysical Research Oceans, 127, e2021JC017581, https://doi.org/10.1029/2021JC017581

⁃ Zhu, Y., Li, Y., Wang, F., Lv, M., 2022: Weak mesoscale variability in the Optimum Interpolation Sea 2 Surface Temperature (OISST)-version 2-AVHRR-only data before 2007, Remote Sensing, 14(2), 409. https://doi.org/10.3390/rs14020409

⁃ Zhu, Y., Li, Y.*, Zhang, Z., Qiu, B., & Wang, F.*, 2021: The observed Agulhas Retroflection behaviors during 1993-2018. Journal of Geophysical Research Oceans, 126, e2021JC017995, https://doi.org/10.1029/2021JC017995

⁃ Duan, J., Li, Y.*, Wang F., Hu, A., Han, W., Zhang, L., Lin, P., Rosenbloom, N., Meehl, G. A. 2021: Rapid Sea-Level Rise in the Southern-Hemisphere Subtropical Oceans. Journal of Climate, 34(23), 9401-9423. doi:10.1175/JCLI-D-21-0248.1

⁃ Guo, Y., Li, Y.*, Wang, F., & Wei, Y., 2021: Ocean Salinity Aspects of the Ningaloo Niño, Journal of Climate, 34(15), 6141-6161.

⁃ Liu, L.-L., Li, Y.*, & Wang, F. 2021: MJO-induced Intraseasonal Mixed Layer Depth Variability in the Equatorial Indian Ocean and Impacts on Subsurface Water Obduction. Journal of Physical Oceanography, 51(4), 1247-1263. doi:10.1175/JPO-D-20-0179.1

⁃ Li, Y.*, Han, W., Wang, F., Zhang, L., & Duan, J., 2020: Vertical Structure of the Upper Indian Ocean Thermal Variability. Journal of Climate, 33 (17), 7233–7253, https://doi.org/10.1175/JCLI-D-19-0851.1

⁃ Guo, Y., Li, Y.*, Wang, F., Wei, Y., & Xia, Q., 2020: Importance of Resolving Mesoscale Eddies in the Model Simulation of Ningaloo Niño, Geophysical Research Letters, 47(14), e2020GL087998, https://doi.org/10.1029/2020GL087998

⁃ Guo, Y., Li, Y.*, Wang, F., Wei, Y., & Rong, Z., 2020: Processes Controlling Sea Surface Temperature Variability of Ningaloo Niño, Journal of Climate, 33(10), 4369-4389, https://dio.org/10.1175/JCLI-D-19-0698.1

⁃ Duan, J., Li, Y.*, Zhang, L., & Wang, F., 2020: Impacts of the Indian Ocean Dipole on Sea Level and Gyre Circulation of the Western Tropical Pacific Ocean, Journal of Climate, 33, 4207-4288.

⁃ Ren, Q., Li., Y, Wang, F., Duan, J., Hu, S., & Wang, F., 2020: Variability of the Mindanao Current induced by El Nino events, Journal of Physical Oceanography, 50(6), 1753–1772.

⁃ Li, Y.*, Han, W., Zhang, L., & Wang, F. (2019). Decadal SST Variability in the Southeast Indian Ocean and Its Impact on Regional Climate. Journal of Climate, 32, 6001-6022.

⁃ Duan, J., Li, Y.*, Wang, F., & Chen, Z. (2019). Multidecadal change of the Mindanao Current: Is there a robust trend? Geophysical Research Letters, 46, 6755–6764.

⁃ Li, Y.*, Han, W., Hu, A., Meehl, G. A., & Wang, F. (2018). Multidecadal Changes of the Upper Indian Ocean Heat Content during 1965–2016. Journal of Climate, 31(19), 7863-7884. 

⁃ Li, Y.*, W. Han, W. Wang, L. Zhang, and M. Ravichandran (2018). The Indian Summer Monsoon Intraseasonal Oscillations in CFSv2 Forecasts: Biases and Importance of Improving Air–Sea Interaction Processes. Journal of Climate, 31, 5351-5370.

⁃ Song, L., Li, Y.*, Wang, F., Wang, J., and Liu, C. (2018). Subsurface structure and variability of the zonal currents in the northwestern tropical Pacific Ocean. Deep-Sea Res., Part I, 141, 11-23.

⁃ Li, Y.*, Han, W., & Zhang, L. (2017). Enhanced Decadal Warming of the Southeast Indian Ocean During the Recent Global Surface Warming Slowdown. Geophysical Research Letters, 44(19), 9876-9884. 

⁃ Li, Y.*, Han, W., Ravichandran, M., Wang, W., Shinoda, T., & Lee, T. (2017). Bay of Bengal salinity stratification and Indian summer monsoon intraseasonal oscillation: 1. Intraseasonal variability and causes. Journal of Geophysical Research: Oceans, 122(5), 4291-4311. 

⁃ Li, Y.*, Han, W., Wang, W., Ravichandran, M., Lee, T., & Shinoda, T. (2017). Bay of Bengal salinity stratification and Indian summer monsoon intraseasonal oscillation: 2. Impact on SST and convection. Journal of Geophysical Research: Oceans, 122(5), 4312-4328.

⁃ Li, Y.*, Han, W., Wang, W., & Ravichandran, M. (2016). Intraseasonal Variability of SST and Precipitation in the Arabian Sea during the Indian Summer Monsoon: Impact of Ocean Mixed Layer Depth. Journal of Climate, 29(21), 7889-7910.

⁃ Li, Y.*, & Han, W. (2016). Causes for intraseasonal sea surface salinity variability in the western tropical Pacific Ocean and its seasonality. Journal of Geophysical Research: Oceans, 121(1), 85-103.

⁃ Li, Y.*, & Han, W. (2015). Decadal Sea Level Variations in the Indian Ocean Investigated with HYCOM: Roles of Climate Modes, Ocean Internal Variability, and Stochastic Wind Forcing. Journal of Climate, 28(23), 9143-9165.

⁃ Li, Y.*, Han, W., & Lee, T. (2015). Intraseasonal sea surface salinity variability in the equatorial Indo-Pacific Ocean induced by Madden-Julian oscillations. Journal of Geophysical Research: Oceans, 120(3), 2233-2258.

⁃ Li, Y., & Wang, F. (2015). Thermocline spiciness variations in the tropical Indian ocean observed during 2003–2014. Deep-Sea Res, Part I, 97, 52–66.

⁃ Li, Y.*, Han, W., Wilkin, J. L., Zhang, W. G., Arango, H., Zavala-Garay, J., . . . Castruccio, F. S. (2014). Interannual variability of the surface summertime eastward jet in the South China Sea. J. Geophys. Res. Oceans, 119(10), 7205-7228.

⁃ Li, Y.*, Han, W., Shinoda, T., Wang, C., Ravichandran, M., & Wang, J.-W. (2014). Revisiting the Wintertime Intraseasonal SST Variability in the Tropical South Indian Ocean: Impact of the Ocean Interannual Variation. J. Phys. Oceanogr., 44(7), 1886-1907.

⁃ Li, Y.*, Han, W., Shinoda, T., Wang, C., Lien, R. C., Moum, J. N., & Wang, J. W. (2013). Effects of the diurnal cycle in solar radiation on the tropical Indian Ocean mixed layer variability during wintertime Madden-Julian Oscillations. J. Geophys. Res. Oceans, 118(10), 4945-4964, doi:4910.1002/jgrc.20395.

⁃ Li, Y., F. Wang and W. Han. (2013). Interannual sea surface salinity variations observed in the tropical North Pacific Ocean. Geophysical Research Letters, 40, 2194–2199, doi:2110.1002/grl.50429. 

⁃ Li, Y., Wang, F., & Tang, X. (2013). Spatial-temporal variability of thermohaline intrusions in the northwestern tropical Pacific Ocean. Science Bulletin, 58(9), 1038-1043.

⁃ Li, Y., & Wang, F. (2013). Thermohaline intrusions in the thermocline of the western tropical Pacific Ocean. Acta Oceanologica Sinica, 32(7), 47-56.

⁃ Li, Y., Wang, F., & Zhai, F. (2012). Interannual Variations of Subsurface Spiciness in the Philippine Sea: Observations and Mechanism. Journal of Physical Oceanography, 42(6), 1022-1038. doi:10.1175/jpo-d-12-06.1

⁃ Li, Y., & Wang, F. (2012). Spreading and salinity change of North Pacific Tropical Water in the Philippine Sea. J. Oceanogr., 68, 439-452.

⁃ Li, Y., Wang, F., & Sun, Y. (2012). Low-Frequency spiciness variations in the tropical Pacific Ocean observed during 2003-2012. Geophys. Res. Lett., 39, L23601, doi:10.1029/2012GL053971. 

⁃ 李元龙; 王凡*; 唐晓晖. 热带西北太平洋热盐入侵的时空变化，科学通报, 2012, (20): 1936.