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刘玉光,博士,男,57岁。中国海洋大学教授/博士生导师,物理海洋学科“海洋环境探测机理与仿真”方向学术带头人,科研方向是物理海洋与海洋遥感。1985年获中国海洋大学硕士学位,1996年获美国特拉华大学博士学位。1990年至2001年先后在美国纽约大学、特拉华大学和南密西西比大学担任访问科学家、研究助理、博士后和研究员,三次获奖。2002-2005年主持了863项目“模块化多源海洋遥感信息融合与同化技术”,参加了“航空遥感多传感器集成与应用技术系统”和“遥感应用模块检测与验证技术研究”等国家级科研课题。2002年至2005年主持了“国家理科基地创建名牌课程项目”教学研究课题,2004年至2005年主持了“山东省高等教育精品课程项目” 一项省级教学研究课题和三项校级教学研究课题。目前指导在读博士生8人,硕士研究生2人。近三年指导的研究生中有三人获得校级优秀研究生奖,一人获得省级优秀研究生奖,二人获得寓新优秀论文奖。发表论文六十余篇,提出的海面斜率概率密度函数模型被编入“随机海浪理论”教科书中。主要论文目录如下:
8 ~2 }6 r5 s, F2 r$ e- gLiu, Y., X.-H. Yan, and M.-Y. Su, 2003: Directional spectrum of wind waves: Part I – model and derivation, Journal of Ocean University of Qingdao, Vol.2,1-12.6 k# z. P% y u L% n2 u/ T: Y
Liu, Y., X.-H. Yan, and M.-Y. Su, 2003: Directional spectrum of wind waves: Part II – comparison and confirmation, Journal of Ocean University of Qingdao, Vol.2,13-24.( l+ g0 V9 D! ?# Z
Liu, Y., M.-Y. Su, X.-H. Yan, and W.T. Liu, 2000: The mean-square slope of ocean surface waves and its effects on radar backscatter. Journal of Atmospheric and Oceanic Technology, 17, p1092-1105.
9 I& G- w' x2 b) @Liu, Y., P.A. Hwang, M.-H. Su, and T.W. Liu, 1998: A new model on equilibrium spectrum of wind waves, Proceedings of the Eight International Offshore and Polar Engineering Conference, Vol. III, p216-221.9 _/ e7 A1 s3 C/ p7 Y3 A8 H% [
Liu, Y., X.-H. Yan, W.T. Liu, and P.A. Hwang, 1997: The probability density function of ocean surface slopes and its effects on radar backscatter. Journal of Physical Oceanography, 27, p782-797.
/ W/ d- ~ U# e& Y0 zLiu,Y. 1996: The spectrum of Gravity-capillary waves, the probability density function of ocean surface slopes and their effects on radar backscatter. Ph.D. Dissertation, published by University Microfilms International, ANN ARBOR, MI, 140pp.0 F! \, W% B( l- n0 R4 f# t$ L
Liu,Y. and X.-H, Yan, 1995: The wind-induced wave growth rate and the spectrum of the gravity–capillary waves. Journal of Physical Oceanography, 25, p3196-3218.' c2 J- F( u; l% A
Liu,Y. and X.-H, Yan, 1994: On the directional behavior of the gravity-capillary waves. 1994 AGU Spring Meeting, Abstract Supplement to EOS, p196.4 x: w. z3 P) t5 v# @8 ~$ I
Liu,Y. and W.J. Pierson, Jr. 1994: Comparisons of scatterometer models for the AMI on ERS-1: The possibility of systematic azimuth angle biases of wind speed and direction. IEEE Transactions on Geoscience and Remote Sensing, 32, p626-635.# O+ b6 A, T6 l* S& I) `2 B' v
Liu,Y., D,Wang and Q.Zhang,1991: The methods of data compression and their application to storage of oceanographic station data. Collect Oceanic Works, 14(1), p38-47.
2 Q- ~- m$ h9 \" e9 ?8 ?+ ~Liu,Y., Z. Yu, and S.Jiang, 1990: Sea current rotary spectrum estimation by the maximum entropy method. Physics of Shallow Seas, p121-129.
8 X9 W- Z4 ~1 K4 KLiu, Y., Z. Yu, and S.Jiang, 1990: Cospectrum and quadrature spectrum estimation by the maximum entropy method. Physics of Shallow7 l* T: O9 s* Q( z' f1 ~* O
Seas, p114-120.* t. i1 o% j( ?4 ~% w' P7 C
Liu, Y., and P. Xiu 2004:Preliminary analysis of ocean-color data observed in the Bohai sea,Serial International Symposium during 80th anniversary of Ocean University of China,Oct. 25-27, 2004, Qingdao, China. p21.
' \9 K% i3 F2 U& Q4 E* UXu,Q., and Y. Liu, 2004:A new formula on the Fresnel reflectance and its application in microwave remote sensing. Science in China,Ser. D Earth Sciences, 2004, 47 (11), 1045-1052.
J( ~4 u# G1 S u9 `/ JXu,Q., Y. Liu, and Lü X., 2005:Adjoint assimilation in marine ecosystem models and an example of application, Journal of Ocean) x9 H# p* t+ |6 U
University of China, 4 (1), 14-20.
b3 x0 g0 {( U) v# a) b eXu,Q., Y. Liu, Lü X. and Cheng Y., 2005: Data assimilation of remote sensed data in a coupled physical-biological model of the Bohai. G& f& c j; |$ p7 H- R A
Sea and the Yellow Sea.
3 ^4 K& c; o& { u1 U- T8 I2 T% r: pAdvances in Marine Ecosystem Modelling Research Symposium, 27-29 June 2005,Plymouth Marine Laboratory (PML), Abstract Book p51, University of Plymouth, Plymouth, UK.) ~8 M8 ?, Y' D1 x' b
Xu,Q., and Y. Liu, 2003:Impact of a New Formula on the Fresnel Reflectance of Microwave Remote Sensing. Proceeding of ACRS 2003 ISRS, The 24th Asian Conference on Remote Sensing & 2003 International Symposium on remote Sensing. ISSN 1226-8743, Vol.1, p372-374. 3-7, November 2003, Busan, KOREA.2 X E/ i2 I, s7 D, N9 P8 H4 h3 p
Yin X., Liu Y., Zhang H.,2005: Removing Wind Direction Impacts on Remote Sensing of Sea Surface Salinity. Chinese Science Bulletin(accepted).
" v q5 }5 z/ K/ h3 r- f9 dYin X., Liu Y.,Wang Z., and Xiu P., 2005:A new algorithm for sea surface salinity retrieval of microwave radiometer. Science in China,Ser. D Earth Sciences(accepted)./ O1 X" P, X4 z, v6 T7 Q
刘玉光,2005:《卫星海洋学》,中国海洋大学教材,259页。
/ p% [; m3 d5 q# A( c徐青、刘玉光,2003:: Y4 l8 v0 F, F$ F; [* o, n% T! G. Q
菲涅耳反射率的一个新公式及其在海洋遥感中的应用, 中国科学(D辑),第33卷,p1103-1111. |# x2 @; `9 ~2 ~" G2 o4 X0 `& n
徐青,刘玉光,程永存,吕咸青,2005:。海洋生态模型中的伴随同化方法。海洋通报(录用)。' b; L; y. [, X* L ~
徐青,刘玉光,
, F' I, U% @, Q3 C程永存,* C4 n4 V" c9 J# t
吕咸青,2005:伴随同化技术在渤、黄海生态模式中的应用:控制变量的选取与孪生实验。高技术通讯(录用)。! T5 e9 d r& Y& H
修鹏、刘玉光,2004:太阳光谱仪的定标技术与渤海海域的光学测量。高技术通讯,第15卷第7期,p85—89,2005.' M! a4 M( |4 ]$ K* F6 n
殷晓斌、刘玉光、张汉德,2005:海表面盐度的微波遥感—平静海面的微波辐射机理研究。高技术通讯,第15卷,第8期,p86-90。
. X' `2 W9 [" F殷晓斌、刘玉光、张汉德,2005:海表面盐度的微波遥感—粗糙海面的微波辐射机理研究。科学通报(录用)。- E5 F- I' Q% k$ c5 _
殷晓斌、刘玉光、王振占、修鹏,2005:一种用于微波辐射计遥感海面盐度的反演算法。中国科学(D辑)(录用)。
3 a, Q, U8 \. }" ~周良明、刘玉光、郭佩芳,2003:多传感器水体参数观测仪AAQ1183及其在海洋水质监测中的应用。气象水文和海洋仪器,第70卷(第4期), p44-57。
V- G" o/ o* j# F, y# r周良明、刘玉光,2003:利用地物光谱仪数据研究水汽对太阳辐射的吸收。海洋技术, 23(4),p109-112.2 H: m5 U! c: w1 F# @
周良明、刘玉光、郭佩芳,2004:关于赤潮水色研究的探讨,海洋湖沼通报, No4, p61-67.
/ C: h+ J# v. N1 d9 P( t( U+ R周良明、刘玉光、郭佩芳,2005:渤海和北黄海水色光谱特征分析,海洋通报,24(2),p13-20。: j7 U; O( D7 Z2 d( n1 D
张军、徐德伦、刘玉光和周良明,2003:ISI921VF水陆两用地物光谱辐射计。高技术通讯,, 2003年第13卷增刊, p33-38。
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刘玉光、汪德元、张芩,1990:数据压缩方法及其在海洋数据存储中的应用,海洋预报,7(2), p65-73。. s# q) u' N3 \- b) x% c! b- q# s
刘玉光、余宙文,1988:旋转谱理论探讨,山东海洋学院学报,18(2), p17-22。% p$ J' |, q. a" r" H( W
刘玉光、余宙文、蒋松年,1987:用最大熵方法研究同相谱和异相谱,海洋学报,9(6), p685-689。
6 M( S- [- j1 B, X/ d% h9 y余宙文、刘玉光、蒋松年,1987:使用最大熵方法估计海流旋转谱,海洋学报,9(5), p544-549。8 q4 J+ J. b& c2 D) s" I0 F
刘玉光、张冬生,1987:海洋气象数据编码转换初探,海洋通报,6(3), p81-89。 |
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