刘玲玲，女，研究员，中国科学院青年创新促进会会员。2008年在中国海洋大学获得物理海洋学博士学位，其后在中国科学院海洋研究所工作至今。主要从事海洋环流动力学及海气相互作用研究。
一、研究领域
海洋环流动力学及海气相互作用研究，包括：海洋垂向环流（潜沉/浮露）动力学及其气候效应，海洋多尺度相互作用和台风-海洋相互作用。
二、招生专业及方向
物理海洋学，海洋环流与气候环境效应
三、研究室及联系方式
中国科学院海洋环流与波动重点实验室
四、承担的主要科研项目
(1) 国家自然科学基金面上项目，全球海洋潜沉/浮露热输送及其变化趋势，2024.01-2027.12 ，主持。
(2) 国家重点研发计划课题，“海气交互关键词浮标观测数据的标准化与示范应用，2022.11-2025.11，骨干。
(3) 国家自然科学基金面上项目， 热带印度洋潜涌率的时空变化特征及季节内振荡的影响，2020.01-2023.12 ，主持。
(4) 国家自然科学基金面上项目， 热带气旋及其变异对北太平洋浅层翻转环流的影响机制，2012.01-2016.12 ，主持
(5) 国家重点研发计划课题 ，区域超高分辨率大气- 陆面耦合模式研制，2017.07- 2020.12，骨干。
五、研究成果及奖励
在国际上首次给出了海洋潜沉/浮露的全球地理格局和由台风驱动的加强区域；扩展了原有的温跃层冬季通风的物理框架和诊断方法，发现在热带海洋季风区亦存在很强的海洋浮露过程；揭示了海洋潜沉/浮露对全球变化的响应规律及其动力学机制，阐明了海洋、大气多尺度动力过程（混合层日循环、海洋中尺度过程、大气季节内振荡等）对潜沉/浮露的影响，填补了潜沉/浮露动力学中诸多的认知空白。
六、代表性论文及著作
(1)Liu, L. L., R. X. Huang, and F. Wang, 2023: Three-dimensional structure of subduction/obduction in the North Pacific Ocean. Journal of Physical Oceanography, 53, 805-820.
(2)Liu, L. L., Y. L. Li, and F. Wang, 2022: Reduction of equatorial obduction by atmospheric intraseasonal oscillations in the western and central Pacific Ocean. Journal of Geophysical Research: Oceans, 127, e2021JC017901, https://doi.org/10.1029/2021JC017901.
(3)Liu, L. L., Y. L. Li, and F. Wang, 2021: MJO-induced intraseasonal mixed layer depth variability in the equatorial Indian Ocean and impacts on subsurface water obduction. Journal of Physical Oceanography, 51, 1247-1263.
(4)Liu, L. L., R. X. Huang and F. Wang, 2020: Ventilation in the South China Sea: Subduction versus obduction. Deep Sea Research I, https://doi.org/10.1016/j.dsr.2020.103227
(5)Hu, S. J., L. L. Liu*, Guan C. et al. 2020: Dynamic features of near-inertial oscillations in the Northwestern Pacific derived from mooring observations from 2015 to 2018. Journal of Oceanology and Limnology, 38(4), 1092-1107.
(6)Zhang, Z. X., L. L. Liu*, and F. Wang, 2019: Oceanic barrier layer variation induced by tropical cyclones in the Northwest Pacific. Journal of Oceanology and Limnology, 37(2), 375-384.
(7)Liu, L. L., R. X. Huang and F. Wang, 2018: Ventilation of a Monsoon-Dominated Ocean: Subduction and Obduction in the North Indian Ocean. Journal of Geophysical Research: Oceans, 123, 4449-4463.
(8)Liu, L. L., R. X. Huang and F. Wang, 2016: Subduction/obduction rate in the North Pacific diagnosed by an eddy-resolving model. Chinese Journal of Oceanology Limnology, 34(4), 835-846.
(9)Liu, L. L., and F. Wang, 2015: Tropical cyclone-induced vertical water transfer and its variability in the North Atlantic and North Pacific. Journal of Oceanology, 71, 401-407.
(10) Liu, L. L., and R. X. Huang, 2012: The Global subduction/obduction rates: their interannual and decadal variability. Journal of Climate, 25, 1096-1115.
(11) Liu, L. L., F. Wang and R. X. Huang, 2011: Enhancement of subduction/obduction due to hurricane-induced mixed layer deepening. Deep Sea Research I, 58, 658-667.
(12) Liu, L. L., R. X. Huang and F. Wang, 2011: The role of diurnal cycle in subduction/obduction. Journal of Oceanology, 67, 273-279.
(13) Liu, L. L., Wang W., and R. X. Huang, 2008: The mechanical energy input to the ocean induced by tropical cyclones, Journal of Physical Oceanography, 38(6), 1253~1266
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