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高迎侠

作者: 添加时间:2020-06-10 09:31:41 浏览:

基本信息

姓名:高迎侠

职称:讲师

所属专业:大气科学

研究方向:季节内振荡;海气相互作用;尺度相互作用

主讲课程:气象统计预报

办公地点:生物楼417

联系方式:yingxiag@qq.com

教育经历:

2013.09–2019.12南京信息工程大学,大气科学学院,气象学,博士(导师:徐邦琪教授)

2009.09–2013.06南京信息工程大学,大气物理学院,雷电防护科学与技术,学士

工作经历:

2020.04–至今bob手办官网安卓版 ,BOB手机版官网 ,讲师

2018.01–2019.01英国雷丁大学,大气科学学院,联合培养博士生

2016.12–2017.02美国夏威夷大学,国际太平洋研究中心,访问学者

主持或参加项目:

1.bob手办官网安卓版 高层次人才引进科研启动基金,主持,2020–2022

2.江苏省研究生培养创新工程项目,主持,高频扰动对季节内振荡的升尺度反馈作用,2016–2019

发表论文:

1.Gao, Y., P.-C. Hsu*, L. Chen, L. Wang, T. Li, 2020: Effects of high-frequency surface wind on the intraseasonal SST associated with the Madden-Julian oscillation.Clim.Dyn.,54: 4485–4498. DOI 10.1175/JCLI-D-19-0337.1

2. Hsu, P.-C.*, Y. Qian, Y. Liu, H. Mirakami,Y. Gao, 2020: Role of abnormally enhanced MJO over the western Pacific in the formation and subseasonal predictability of the record-breaking Northeast Asian heatwave in the summer of 2018.J. Climate, 33: 3333–3349. DOI: 10.1175/JCLI-D-19-0337.1

3.Gao, Y., P.-C. Hsu*, T. Li, 2019: Effects of high-frequency activity on latent heat flux of MJO.Clim. Dyn., 52: 1471–1485. DOI 10.1007/s00382-018-4208-1

4.Gao, Y.*,N. P. Klingaman, C. A. DeMott, P.-C. Hsu, 2019: Diagnosing ocean feedbacks to the BSISO: SST-modulated surface fluxes and the moist static energy budget.J. Geophys. Res.-Atmos., 124: 146–170. DOI 10.1029/2018JD029303

5. DeMott, A. C.*, N. P. Klingaman, W-L. Tseng, E. A. Burt,Y. Gao,D. A. Randall, 2019: The convection connection: How ocean feedbacks affect tropical mean moisture and MJO propagation.J. Geophys. Res.-Atmos., 124(22): 11910–11931. DOI 10.1029/2019JD031015

6. He, Z., P.-C. Hsu*, X. Liu, T. Wu,Y. Gao, 2019: Factors limiting the forecast skill of the boreal summer intraseasonal oscillation in a subseasonal-to-seasonal model.Adv. Atmos. Sci., 36(1): 104–118. DOI 10.1007/s00376-018-7242-3

7.贺铮,徐邦琪*,高迎侠, 2018: BCC S2S模式对亚洲夏季风准双周振荡预报评估.应用气象学报, 29(4): 436–448. DOI 10.11898/1001-7313.20180405

8.Gao, Y., P.-C. Hsu*, H.-H. Hsu, 2016: Assessments of surface latent heat flux associated with the Madden-Julian Oscillation in reanalyses.Clim. Dyn., 47: 1755–1774. DOI 10.1007/s00382-015-2931-4

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