邢久星研究员

电话:(86)-755-26036322  
邮箱:jxx2012@sz.tsinghua.edu.cn 办公地址:深圳大学城清华校区海洋楼,1215室,邮编:518055

所属学科:海洋科学

【个人简历】

1978年2月~1982年2月, 南京气象学院(现南京信息工程大学),气候,本科毕业

19859~19887月,气象科学研究院,气象,硕士毕业

19889~19922月,英国雷丁大学,物理海洋,博士毕业

19822~19859月,国家气象局气象科学研究院工作

19922~20133月,英国国家海洋中心(前普劳德曼海洋研究所)工作

20147~现在,澳门赌场网站_手机赌博网址工作

【研究领域】

在大陆架海洋动力学研究,数值模型的发展及应用都有重要成果和贡献。其中,首次建立了爱尔兰海的斜压模式,对锋面和冷水团的动力学过程成功地进行研究;首次利用数值模型对苏格兰海大陆架边缘过程,特别是内潮,内波和近惯性内波进行研究,取得重要进展。对海洋动力学,特别是大陆架物理过程,如湍流和内波,潮及内潮,近海环流,以及锋面等具有深入研究。以第一作者身份发表SCI论文五十余篇,其中在本专业最顶级的JPO, GRL 和JGR上共发表二十余篇。在研项目:南海亚中尺度涡(973子课题), 深圳近海风暴潮(深圳科创委)。

【最近论文】

[1] Xing, J. and S. Chen (2017). A process study of the interaction of tidal currents, tidal mixing and density gradient in a region of freshwater influence. Journal of Marine Systems, 172 (2017) 51-63.

[2] Chen S., J. Xing and D. Chen (2017). A study on some basic features of inertial oscillations and near-inertial internal waves. Ocean Sciences, 13, 829-836, 2017

[3] Yang Y., J. Xing, D. Chen and S. Chen (2017). A modelling eddy-splitting by an island/seamount. Ocean Sciences, 13, 837-849, 2017

[4] Xing J., A. M. Davies and E. Jones (2012). Influence of sea surface wind wave turbulence upon wind induced circulation, tide-surge interaction and bed stress. Ocean Dynamics 62(7). 1017-1042. 10.1007/s10236-012-0542-8.

[5] Xing J., A. M. Davies and E. Jones (2011).  Application of an unstructured mesh model to the determination of the baroclinic circulation of the Irish Sea. Journal of Geophysical Research – Oceans, Vol. 116, C10026, doi:10.1029/2011JC007063.

[6] Xing, J. and A. M. Davies (2011). On the interaction of internal tides over adjacent sills in a fjord. Journal of Geophysical Research – Oceans, VOL. 116, C044022, DOI 10.1029/2010JC006333.

[7] Xing, J., E. Jones, A.  M. Davies and P. Hall (2011). Modelling tide-surge interaction effects using finite volume and finite element models of the Irish Sea. Ocean Dynamics. DOI 10.1007/s10236-011-0418-333.

[8] Xing, J. and A. M. Davies (2009). Influence of multiple sills upon internal wave generation and the implications for mixing. Geophysical Research Letters,36, L13602, doi:10.1029/2009GL038181.

[9] Xing, J. and A. M. Davies (2009) Influence of bottom friction effects in sill regions upon lee wave generation and implications for internal mixing. Ocean Dynamics, DOI 10.1007/s10236-009-0215-4.

[10] Berntsen J., J. Xing and Alan M. Davies (2009). Numerical studies of flow over a sill: sensitivity of the non-hydrostatic effects to the grid size. Ocean Dynamics, DOI10.1007/s10236-009-0227-0.

[11]Xing, J. and Davies, A.M. (2006). Processes influencing tidal mixing in the region of sills.  Geophysical Research Letters, 33, L04603, doi:10.1029/2005GL025226.

[12] Xing, J. and Davies, A.M. (2006). Influence of stratification and topography upon internal wave spectra in the region of sills.  Geophysical Research Letters, 33, L23606, doi:10.1029/2006GL028092.

[13] Xing, J. and Davies, A.M. (2006). Internal wave trapping and mixing in a cold water dome, Journal Geophysical Research, 111, C07002, doi:10.1029/2005JC003417.

[14] Berntsen J., Xing, J. and Guttorm A. (2006). Assessment of non-hydrostatic ocean models laboratory scale problems. Continental Shelf Research, 26 (12-13), 1433-1447, doi: 10.1016/j.csr.200602.014.

[15] Xing, J. and Davies, A.M. (2004). Modelling non-linear interaction between wind forced flows in surface frontal regions.  Geophysical Research Letters, 31, L11308, doi:10.1029/2004GLO19490.