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师资介绍 黄瑞新教授

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黄瑞新教授 * V$ I" {' z& M" @# n& U. _ + J, `1 I. S+ ` 0 Z% E) T. \+ n% D0 r! Z- ZRui Xin Huang* @3 @; B P& x+ N, |; ?; m+ y 6 I5 m0 ?7 [/ R5 _: O0 F Senior Scientist . R5 V( H( S7 q: M9 q& ~& aW. Van Alan Clark, Jr., Chair for Excellence in Oceanography, 2002-; 1 G( w! J) z% @5 I3 e. pWoods Hole Oceanographic Institution $ A9 i( `. y. O% R! T6 h 6 e. q B( ]5 ?Phone: (o) 508-289-2532; % F G d7 g* M) u1 h6 u, oFAX: 508-457-2181; ( K' ^5 m5 o9 Z2 A/ {e-mail address: rhuang@whoi.edu3 \. {( _/ d0 U" g( Y4 R$ W Date of Birth: Sep. 15, 1942: _) }5 h9 ~$ ~! x& t% m$ w" h Citizenship: U.S.A. ! _+ n3 E% Y! a9 {/ { ' }1 V r$ ~% t9 R' }( x$ p, TEducation 8 ?$ L# f8 y/ y; e# p& e) d: ? 7 T, f8 n+ |$ ?8 p' u ]# i# E1 a7 ~The University of Science and Technology of China, 1960-65; B.S. in % V1 |+ l( O/ ]7 W2 t1 Z$ IThermo-physical Fluid Dynamics of Jet Propulsion, 1965.7 M$ `0 Y' t, N ; i+ Q3 x$ v8 S) d. ?& N- Y Graduate School, University of Science and Technology of China, Meteorology, 1978-80. $ t3 H( X) g* i2 z; i( W 5 I" j' } M( f! h5 \% A. }The Johns Hopkins University, Geophysical Fluid Dynamics, Sep. 1980-Feb. 1981. 5 K/ s; ~$ f. {- K; ^) g 1 Y3 i; a- u1 u4 f7 @Massachusetts Institute of Technology/Woods Hole Oceanographic Institution, 1981-1984; Ph.D. in Physical Oceanography 1984. : R; Q& @6 H, i * z- D7 s7 t: u, f" PExperience 2 c# q. f2 j- v3 g7 @; T0 T& x, G8 T% N! ~ Research Associate, Institution of Mechanics, Beijing, China, 2 C9 ?. ^# m4 Z2 _% b b7 B$ }9 C! f8 | n s: v 1965--1978. Self-study of English and mathematics during the ' d0 r/ i X: A% W; M8 I& f3 c0 BCultural Revolution in China; aerodynamics of wings; transonic flow in 6 T6 ?! K# C; `- d- V Turbo-machine; design of transonic turbo-machine; design and build the first transonic cascade tunnel in China; translation of a large five-language dictionary in physics.- U- t$ Y. `- X $ a2 U H9 h7 ] Postdoctoral, M.I.T., 1984. , L' |2 }' w& t4 F1 B+ b W Visiting Scientist, Geophysical Fluid Dynamics Laboratory (NOAA), Princeton University, 1984--1986, March--June 1992.) L7 d* c3 x: N 3 R7 \: B( U( |" P$ [# q; ^# h Assistant Scientist, 1986--1990; Associate Scientist, 1990-1998; tenure awarded, 1993, Senior Scientist, 1998-, Woods Hole Oceanographic Institution; 7 S3 M7 l* ~& |. m9 j7 b" k+ g" P9 d ) B! b8 @: e7 l, |( FVisiting Associate Professor, University of Hawaii, Jan.-June, 1994.* R1 l; o2 x! j* P' r9 b 1 m& o9 Z f- ^# m& G% W- \! l Visiting Scientist, Cooperative Institute for Marine and Atmospheric Studies,7 S9 R2 W$ Q% v* g3 W0 j University of Miami, Feb., 1999.) H M% K2 t# e! L. k. \ * t4 c8 y4 r* j! _0 n- | Visiting Professor, Lamont-Doherty Earth Observatory, Columbia University, March-May., 1999.8 n) Q5 d( b$ _) N+ R; W3 O : t' a1 a. C& m4 Q8 O( Z Corresponding Member, U.S. WOCE Working Group on Numerical Modeling, 1989-1992.$ _6 z) E) j* R2 J! r# m 6 }1 ^' n$ l8 y% u M PJoint Committee of Physical Oceanography, MIT/WHOI Joint Program, 1990-93.2 p& t. @+ Z1 U* b! f, [ - R/ R( h- d+ p4 W Member, Working Group on Oceanic Thermohaline Circulation and Variability, 4 U. Z/ C* u; D* @0 dClimate System Modeling Project, USA, 1993-96. : A+ ^( M' e' I; R) l) B0 P0 l V+ h% v! N1 G0 [! H( Y Member, Climate Change Committee, WHOI, 1995-1999. 5 H0 y* x2 ~/ t4 l. j3 U7 ^1 {$ E( Y3 o6 ]+ r) E3 o& i0 Q* l' X Member, Advisory Committee, Ocean and Climate Change Institute, 2001-2005. ( c# X- ^1 T M% j8 E; ]: A, H6 l& }$ S, a; {4 p& D5 h Guest Professor, Ocean University of Qingdao, China, 1996--.* l% B2 z4 n% h. d; I' J3 V P% O 4 L3 v! R f5 S7 T: o6 ^ Chairman, Academic Committee for the national Key Laboratory of Physical Oceanography, Ocean University of China, 1999-2005.) ?$ \7 M" q4 a/ _7 m) e ; G( j) p- i u( L+ z( y) wMember, Advisory Academic Committee of the National Key Laborotory of numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, 2001- 2005. , }. @; ]7 O! J/ Z7 _& D ' P+ _8 d8 c4 s7 ~) JGuest professor, South China Institute of Oceanology, Chinese Academy of Sciences, 2002-.+ y# c: o( k- q2 C+ d ( y) a3 T8 D3 u2 n3 h# D _; ]4 P 8 X+ P4 R4 H& {4 t* |0 `% STeaching- k# q& x5 L. H" E 6 ~+ G8 @) V& Y! r+ v' [Steady Circulation in the Oceans and Atmosphere, MIT/WHOI Joint Program, 1988-1991. ' l0 r: A) p3 s8 c+ F 1 q/ t3 i" p, J# V1 HRecent Advances in Large-Scale Ocean Circulation Theory, Second Institute of Oceanography, Hangzhou, China, October 7-17, 1992. ' m: N5 B5 d2 p6 N, @6 ^0 X3 n' E( w) [' ^ Theories of the Oceanic General Circulation, University of Hawaii, Spring, 1994., Y, R- @/ {* R- ^7 X - m9 n# [4 E% ?Advances in Theories of Wind-Driven and Thermohaline Circulation, International 8 p9 t( h6 n s6 f# n } " c9 S+ F5 E6 r+ `# K2 a" wSummer School on Ocean-Atmosphere Interaction, July 25-August 4, 1994, Qingdao, China. % w6 S( ~' [4 z& f. F- ? ! }9 H8 f: d3 t0 N7 U9 ]Theories of the Oceanic General Circulation, MIT/WHOI Joint Program, 9 c$ g4 ]' A" z) o( a1 t' F0 Z) f4 O8 o. a8 |7 X Spring 1995, Fall, 1998, Fall, 2001, Spring, 2004. & {" K, U7 m/ w+ u8 {! P- H- Z! N9 u1 N$ y6 T: X; G Supervision1 H# U& T w9 y5 W2 H 0 V2 ^3 |; B4 O& j3 R r Served as a mentor for Dr. Krupitsky (Institution Postdoctoral Fellow), Dr. Mahdi Ben Jelloul (Institutional Postdoctorial Fellow), Dr. Jiayan Yang (when he was an Assistant Scientist).$ F5 I3 e" j2 n1 o0 `0 I 5 z0 {. F. }% b N, W: O Mr. James McLaren, 1987-89; Mr. Li Ping Wang, 1989-93 (Ph.D.); 8 `( K+ o' Z% P6 ]5 }2 R ' b4 a& Y+ a6 U$ X3 p3 ` On thesis committee of other six students, chairman of thesis defense committee for Mr. Hui Ming Zhang and Ms. Sarah Gille. 4 @) C' x) L0 j1 h, U ; ~" n7 t2 O- Z) [( SMichael Masterson, Summer Student Fellow, 1987; Marcel Lieberman, Summer Student1 F7 _2 w1 c7 O5 w5 ? Fellow, 1989; Sarah Russell, Summer Student Fellow, 1993. 2 {" G; H' |. L # b+ G/ d e* C; T" QSea Cruises+ ? h9 O" q7 a8 _, `. F$ e / e3 J5 @! T+ X4 h; xRV OCEANUS, Seasor test cruise, July, 1989. 2 Z6 b. V) q9 r9 jOceanus, Immerges Sea Cruise, August, 2003. ( V9 W8 d, L! H( u% M! a5 Y9 j 7 \- L. {, F u u& G# m Honor $ H4 k$ A3 E: i* w! q. M+ h8 ^3 A( [5 G Nominee of President Young Investigator Award, 1989. % @1 x/ }& V1 j. m8 L3 y3 [3 S , d% Y6 K* Q& {" x* _6 {0 BResearch Interest:4 u; f5 Y! L5 e2 U% k 0 w: o. B s/ r( w: w6 u Theoretical and numerical studies of the wind-driven and thermohaline circulation in the oceans, dynamics of western boundary currents, flow over topography, climate and paleoclimate dynamics. * r |" u. r G, h, O8 } A4 O+ f7 t: q8 V Author or co-author of 70 refereed scientific publications.' G4 t/ r: A3 y4 T( ?8 _ 8 O }$ A7 Q' e, \7 wRefereed Publications * A! E2 }. G( ~$ l; }6 ~" i* q2 O0 j0 K3 I, p2 _+ G Huang, R. X. and J. P. Chao, 1980. A linear theory of spiral cloud bands of typhoon. Scientia Atmospherica Sinica, 4, No. 2. (in Chinese with English Abstract).5 I7 `3 F3 [6 D( k 6 E% T& Z }4 r0 | Chao, J. P. and R. X. Huang, 1980. The cnoidal waves of a rotating barotropic atmosphere.   Scientia Sinica, XXIII , No. 10, 1266--1277.6 _( f [) ]5 J2 a% b 5 K. q0 p9 L7 D* s( B- D Huang, R. X., 1986. Solutions of the ideal fluid thermocline with continuous stratification.   J. Phys. Oceanogr., 16, 39--59. ! b% L5 h( A( N( ]: j+ j( M- |3 d( c! y6 A0 y! K4 H- y* N Bogue, N. M., R. X. Huang, and K. Bryan, 1986. Verification experiments with an isopycnal coordinate ocean model. J. Phys. Oceanogr., 16, 985--990. , o* j! B9 t0 P2 q6 d " O* }* o+ D. f, ^" l- ], ^Huang, R. X., 1986. Numerical simulation of wind-driven circulation in a subtropical-subpolar basin. J. Phys. Oceanogr., 16, 1636--1650.- R1 m1 Q G" E/ H( m 7 O: J2 E/ q1 C% m# }8 Y, G Huang, R. X., 1987. A three-layer model for wind-driven circulation in a subtropical-subpolar basin. Part I: Model formulation and the Sub-critical state.   J. Phys. Oceanogr., 17, 664--678.* Z( k/ H. t! r1 s7 Q1 Y 0 Y* U, I* l0 m# ]7 ^9 Q! B3 eHuang, R. X., 1987. A three-layer model for wind-driven circulation in a subtropical-subpolar basin. Part II: The supercritical and hypercritical states. J. Phys. Oceanogr., 17, 679--697. 5 B; Q. x" J% @7 e& C3 z4 t# i' I( V; P* l" v Huang, R. X. and G. R. Flierl, 1987. Two-layer models for the thermocline and current structure in subtropical/subpolar gyres. J. Phys. Oceanogr., 17, 872--884. 6 K2 J# \/ x& w9 o: \: d$ z+ q* B) Y Huang, R. X. and K. Bryan, 1987. A multi-layer model of the thermohaline and wind-driven ocean circulation. J. Phys. Oceanogr., 17, 1909--1924. 4 J& ~, o/ x$ e& D, z* ^( O; h# F5 W& c2 A M% R/ y3 n8 @ Huang, R. X., 1988. On boundary value problems of the ideal-fluid thermocline.   J. Phys. Oceanogr., 18, 619--641.* @1 S, P, c& d- m" V 1 p7 ]% O4 D2 B/ u# K% _, V3 b- ?- XHuang, R. X., 1988. Ideal-fluid thermocline with weakly convective adjustment in a subpolar basin. J. Phys. Oceanogr., 18, 642--651. : M- {) z2 A$ `+ [* d , S- T( Y3 I7 a, A% p# w: vHuang, R. X., 1988. A three-layer model for wind-driven circulation in a subtropical-subpolar basin. Part III. Potential vorticity analysis. J. Phys. Oceanogr., 18, 739--752. . [: n3 @" `2 o* a# B! S. c: ]3 E; o p5 D/ s' z Huang, R. X., 1989. The generalized eastern boundary conditions and the three-dimensional structure of the ideal fluid thermocline. J. Geophs. Res., 94(C4), 4855--4865.% s9 Y [$ S0 w9 O; e % x" s7 z2 m. f9 @- FHuang, R. X., 1989. Simulating the main thermocline in the North Atlantic with an ideal-fluid model.   J. Phys. Oceanogr., 19, 543--547.8 |+ s2 [, X- F2 q. f6 P + O$ `8 g, N/ u% U" O) c1 J Huang, R. X., 1989. Sensitivity of a multi-layered oceanic general circulation model to the sea surface thermal boundary condition. J. Geophs. Res., 94(C12), 18,011--18,021. 0 m5 i6 e3 U4 ~8 B5 e+ f! i3 c1 h7 l6 K Huang, R. X., 1990. Does atmospheric cooling drive the Gulf Stream recirculation?   J. Phys. Oceanogr., 20, 750--757." @' }$ S) p. H/ a8 T a 6 Z7 r8 x+ {% q! I7 l. J' D7 f Huang, R. X., 1990. On the three-dimensional structure of the wind-driven circulation in the North Atlantic. Dynamics of Atmospheres and Oceans, 15, 117--159.; [! E& ^9 {8 B' u7 f# o. D + U. z |$ m6 z, e+ G Huang, R. X., 1990. On the structure of inertial western boundary currents with two moving layers.   Tellus, 42A, 594--604. ' M$ ]# h& r2 F- M' R |8 _5 {9 `, K+ v. X- G Huang, R. X. and H. M. Stommel, 1990. Cross-sections of two-layer inertial Gulf Stream.   J. Phys. Oceanogr., 20, 907--911. ' S9 M9 a, c2 |$ x3 I1 V+ z0 V6 U Huang, R. X., 1990. Matching a ventilated thermocline model with inertial western boundary currents.   J. Phys. Oceanogr., 20, 1599--1607. ' X- A9 U, Y2 M' }4 N- n6 N+ _ / W+ p& H8 Y& ` Huang, R. X., 1991. A note on combining wind and buoyancy forcing in a simple one-layer ocean model.   Dynamics of Atmospheres and Oceans, 15, 535--540.' p) \- Y* U: V% u9 Y" a+ C 4 e3 x% F& z9 A9 T5 A. a3 tHuang, R. X., 1991. The three-dimensional structure of wind-driven gyres: ventilation and subduction.   U.S. National Report to International Union of Geodesy and Geophysics 1987--1990, Supplement to Reviews of Geophysics, 590--609. 5 N+ T( y. P* p1 E4 [3 i 4 [; g# S1 V% v/ dHuang, R. X., J. Luyten, and H. M. Stommel, 1992. Multiple equilibrium states in combined thermal and saline circulation. J. Phys. Oceanogr., 22, 231--246./ v6 ^4 v& N/ n( o& K) X7 \ % D7 s* z j- \ @. e2 s0 D2 bHuang, R. X. and H. M. Stommel, 1992. Convective flow patterns in a eight-box cube driven by combined wind stress, thermal, and saline forcing. J. Geophs. Res., 97(C2), 2347--2364. 4 o, ~' E. G: x# H& m2 @. x: B5 b0 {1 l0 T" _/ v Lin, R. Q., R. X. Huang, and J. R. Apel, 1992. A study of the astronomical theory of ice ages in a two-dimensional nonlinear climate model.   J. Geophs. Res., 97(D9), 10,029--10,036.0 L9 t8 a' {5 Y- u * X! m% ~0 d4 c7 T Huang, R. X., 1993. A two-layer model for the wind and buoyancy forced circulation. J. Phys. Oceanogr., 23, 104--115.0 K; R U: W# }0 t& z ( B4 j3 I8 F+ t; ` o0 Z Huang, R. X. and R. W. Schmitt, 1993. The Goldsbrough—Stommel circulation of the world oceans.   J. Phys. Oceanogr., 23, 1277--1284. ; @0 l) `+ h" r1 `2 G$ d/ l 8 Z7 C# f$ e. `/ c' t" THuang, R. X., 1993. Real freshwater flux as a natural boundary condition for the salinity balance and thermohaline circulation forced by evaporation and precipitation. J. Phys. Oceanogr., 23, 2428--2446.: P: O* R* N1 S- @1 | 3 M$ g0 D* e, l0 b4 q/ v8 O Huang, R. X. and H. Stommel, 1993. The globe on a heart-shaped map. In "New equal area world map projections to better display polar regions," by Athelstan Spilhaus, Proceedings of the American Philosophical Society, 137, (2), 181-184.% l2 h$ O B {+ y 2 }4 \! e& t" ?3 C# N) [Huang, R. X. and R. L. Chou, 1994. Parameter sensitivity study of the saline circulation. Climate Dynamics, 9, 391-409./ X* u- k, m4 C8 Y: X 5 F$ ^+ m# }" u. p3 _5 { Huang, R. X., 1994. Thermohaline circulation: Energetics and variability in a single-hemisphere basin model. J. Geophs. Res., 99, (C6), 12,471-12,485.5 C; d# ~) t) a& a4 z7 n2 ^+ \ % P* ~0 R, S3 W# U/ a' Z Huang, R. X. and B. Qiu, 1994. Three-dimensional structure of the wind-driven circulation in the subtropical North Pacific. J. Phys. Oceanogr., 24, 1608-1622. : z1 w4 e! f- ~, v 0 F! t5 D, q- f/ u2 gWang, L. P. and R. X. Huang, 1994. A simple model of abyssal circulation in a circumpolar ocean. J. Phys. Oceanogr., 24, 1040-1058. # o7 C: `/ ]7 k" d x! ?+ _9 U6 X& B) A! n Huang, R. X. and S. Russell, 1994. Ventilation of the subtropical North Pacific. J. Phys. Oceanogr., 24, 2589-2605. " C& J! {9 b( y5 L0 Y4 u0 k/ ~8 f G! x0 p* f Wang, L. P. and R. X. Huang, 1995. A linear homogeneous model of wind-driven circulation in a -plane channel.   J. Phys. Oceanogr., 25, 587-603.1 z6 d5 S1 I- @& S0 ?' I+ Y 9 Z6 B( p1 z; ]Dewar, W. K. and R. X. Huang, 1995. Fluid flow in loops driven by freshwater and heat fluxes.   Journal of Fluid Mechanics, 297, 153-191. * i0 ~$ h; l& u# o; ? ) h# ~2 o/ s1 n8 j2 L/ b: c9 `Pickart, R. and R. X. Huang, 1995. Structure of an inertial deep western boundary current. Journal of Marine Research, 53, 739-770.5 v* T/ R3 l% N * x7 [8 b% c5 ~- f9 t H7 Y- | Qiu, B. and R. X. Huang, 1995. Ventilation of the North Atlantic and North Pacific: Subduction vs. Obduction. J. Phys. Oceanogr., 25, 2374-2390.4 d9 D) e5 C o6 F* J& K$ ~ / T1 i; x8 o5 i6 V L Huang, R. X. and J. R. Luyten, 1996. Reply. J. Phys. Oceanogr., 26, 286. " x0 x7 L) X! X7 w % s( k2 u( S. R Dewar, W. K. and R. X. Huang, 1996. On the forced flow of salty water in a loop. Physics of Fluids, 8, 954-970. 5 f7 A$ H4 V# b7 ?+ C3 x3 b. `7 M& Q. ` Yang, J. and R. X. Huang, 1996. Decadal oscillations driven by the annual cycle in a zonally-averaged coupled ocean-ice model. Geophysical Research Letters, 23, 269-272., E E) k0 s7 g$ L4 V9 C 3 s, H; Q2 u" ?) d' }. w/ ?7 Z3 V' L$ l0 |- ? Huang, R. X. and W. K. Dewar, 1996. Haline circulation in a loop model: bifurcation and chaos.   J. Phys. Oceanogr., 26, 2093-2106./ |5 `( a# T9 Z, @ ! e+ g% ^' z$ }3 p/ ~1 B3 F Huang, R. X. and J. Yang, 1996. Deep-water upwelling in the frictional western boundary layer. J. Phys. Oceanogr., 26, 2243-2250. ! m6 ^& U: E1 C1 |( c2 X) ^8 m# w3 N- X. l! A6 I Huang, R. X., 1998. Available potential energy in a Boussinesq ocean, J. Phys. Oceanogr., 28, 669-678.7 ~; y, w I0 S N4 r+ _ - t, q. {6 q( U* L3 ^0 AHuang, R. X., 1998. On the energy balance of the oceanic general circulation.   Chinese Journal of Atmospheric Science, 22, 452-467.. c& p/ P( b1 B6 G8 F 9 W1 I8 ?. P6 y7 b: JHuang, R. X. and Bo Qiu, 1998. The structure of the wind-driven circulation in the Subtropical South Pacific Ocean, J. Phys. Oceanogr., 28, 1173-1186.$ x% Q0 {6 U; v- A 3 q7 d! N% J% P9 l Wang, L. and R. X. Huang, 1998. A homogeneous model of the Decon cell in a circumpolar ocean. Dyn. Atmos. Oceans, 28, 157-177. 3 U6 n- F% \$ n c- X & @* a- r i9 t: a% cZhang, J., R. Schmitt, and R. X. Huang, 1998. Sensitivity of the GFDL Modular 2 c% F1 W- }/ n8 ?' I7 n: ?+ p0 o4 pOcean Model to parameterization of double-diffusive processes, J. Phys. Oceanogr., 28, 589-605. 0 ]7 z1 R, ~- y2 ~. _: R6 A$ ^1 ] + I9 _7 y5 g# f% v5 S5 ?1 R5 t Kelly, K. A., S. Singh, and R. X. Huang, 1999. Seasonal variations of sea surface height in the Gulf Stream region. J. Phys. Oceanogr., 29, 313-327.7 w, |* m( f/ R D8 Y 9 Y; J% H R- l$ u1 ^8 D& K! v QHuang, R. X., 1999. Mixing and energetics of the thermohaline circulation.   J. Phys. Oceanogr., 28, 727-746. 6 r! G$ A$ k0 a8 p2 T: _% Q$ X$ u9 O8 K9 g; P& f# p Zhang, J., R. Schmitt, and R. X. Huang, 1999. The relative influence of diapycnal mixing and hydrologic forcing on the stability of thermohaline circulation, J. Phys. Oceanogr., 29, 1096-1108. ) S( _! M* ?5 v, v, j4 ^ : S7 D- e4 \7 ^% l Jin, X.-Z., R. X. Huang, and J.-Y. Yang, 1999. Centennial oscillations in an ocean-ice coupled model. Adv. Atmos. Sci., 16(3), 323-342. Q/ N: J/ r" ~4 N" ]' v; B 0 I1 h5 e) o( h+ e Huang, R. X. and J. Pedlosky, 1999. Climate variability inferred from a layered model of the ventilated thermocline, J. Phys. Oceanogr., 29, 779-790.- A8 I8 H# B% E, F 0 G9 e" K3 h. E! ~/ I+ q, { Huang, R. X., 2000. Climate variability inferred from a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 389-1406. 9 ?9 V8 z0 M5 ~3 n9 ]' L) v ; q' s3 P* h5 F( _7 E. bHuang, R. X., 2000. Parameter study of a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 1372-1388. 9 V3 P- i' c6 x0 G 0 z) ?1 @8 _; S1 v, N1 _3 v& q; A Huang, R. X. and J. Pedlosky, 2000. Climate variability of the equatorial thermocline inferred from a two-moving-layer model of the ventilated thermocline, J. Phys. Oceanogr., 30, 2611-2626. , Z9 V, G! N! E4 d! e' U! Y4 r! [ Huang, R. X., and J. Pedlosky, 2000b: Climate variability induced by anomalous forcing in a multi-layer model of the ventilated thermocline. J. Phys. Oceanogr., 30, 3009-3021. ( o/ M; u0 y, d0 [9 S. @ ' T2 _0 c/ T9 OHuang, R. X., M. A. Cane, N. Maik, and P. Goodman, 2000. Global adjustment of the thermocline in response to deepwater formation. Geophysical Research Letter, 27, 759-762. ! u! Y3 O7 _+ s5 e7 s8 R3 [* y% x/ ~; u% t1 l2 Y7 e' T, b Huang, R. X., X.-Z. Jin, and X.-H. Zhang, 2001. An ocean general circulation model in pressure coordinates. Advances in Atmospheric Science, 18, 1-22.& w9 {$ H/ n! x4 j: P 3 H$ s. C, K# o, P! E( Z# Z Huang, Rui Xin, 2001. An analytical solution of the ideal-fluid thermocline. J. Phys. Oceanogr., 31(8), Part 2, 2441-2457. . b' D% V: ]! ^" G3 Q! V$ Z ' s7 w6 p" V: t& U/ C1 H% }2 yDewar, W. K, and R. X. Huang, 2001. Adjustment of the ventilated thermocline. J. Phys. Oceanogr., 31, 1676-1697. : j: d& @ A% F4 b. e; ~! K- h0 k$ g; u- ^. n5 {+ G# S Y" d& f Huang, R. X., and Q. Wang, 2001: Interior communication from the subtropical to the tropical oceans. J. Phys. Oceanogr., 31, 3538-3550. 6 \- y/ i0 a- S6 E+ }1 v: g1 {' Y% ?% ? Huang, R. X., 2001. The available potential energy in a compressible ocean. In P.F. Hodnett (Ed.) IUTAM Symposium on Advances in Mathematical Modeling of Atmosphere and Ocean dynamics, Pp167-172. + o; L4 n9 h& J( I4 ^' v % W1 y. U) h( L1 `" yHuang, R. X. and J. Pedlosky, 2002. On aliasing Rossby waves induced by asynchronous time stepping. Ocean Modelling, 5, 65-76. " Z K2 j+ Z8 X& \" x# v 7 W' C Z" h4 Q- K! s* HHuang, R. X. and X.-Z. Jin, 2002. Deep circulation in the South Atlantic induced by bottom-intensified mixing over the mid-ocean ridge. J. Phys. Oceanogr., 32, 1150-1164. 8 _& R& @- X" c0 K1 S8 G; N ) S7 L$ X# L; b% r Huang, R. X., and X.-Z. Jin, 2002. Sea surface elevation and bottom pressure anomalies due to thermohaline forcing: Part I: isolated perturbations. J. Phys. Oceanogr., 32, 2131-2150. * j% F4 A. p$ }! e 4 H4 a" I: f7 i% z- P0 y8 IZhang, X.-H., W. Li, X.-Z. Jin, and R. X. Huang, 2002. The development of an oceanic general circulation model based on the pressure coordinates and its application. Advances in Natural Science, 12, 1015-1020. (in Chinese). 7 U R- j0 P' _* g% Z2 q$ l1 b+ l" V0 ^& r& r* D) G2 Z Huang, R. X. and F. F. Jin, 2003. The asymmetric nature of the equatorial undercurrent in the Pacific and Atlantic. J. Phys. Oceanogr., 33, 1083-1094.# D9 c( o/ h+ b9 O " I0 w. E2 F; [. _1 W) X! P7 fWang, W. and R. X. Huang, 2004. Wind energy input to the Ekman Layer. J. Phys. Oceanogr., 34, 1267-1275. 4 b0 _: z+ X4 s8 q: m4 ?4 d5 { 9 j8 z8 @7 `' ^2 Y+ XWang, W. and R. X. Huang, 2004. Wind energy input to the surface waves. J. Phys. Oceanogr., 34, 1276-1280.. z/ ~/ |4 ?! E- ]) `0 C 6 n( t |) a- Z! D- a7 T/ u. dHuang, R. X., 2004. Ocean, energy flow in. C. J. Cleveland (Ed.) Encyclopedia of Energy, Elsevier, Vol. 4, pp 497-509. 1 k8 }, T! s: q% n( s; E& n4 e: |8 ?- [6 r# R' ` Huang, R. X., 2005: Available Potential Energy in the World Oceans, J. Mar. Res., in press. 7 R* R% [0 g. D% Q# Z. C2 @: U D# m% q4 l3 y Wang, Q. and Rui Xin Huang, 2005: Decadal Variability of Pycnocline Flows from the Subtropical to the Equatorial Pacific, J. Phys.Ocanogr., in press.3 I* p% n, v, r" ~3 K3 o) m1 f: c, Q) H & X3 f8 _3 d3 ^, m. rWang W. and R. X. Huang, 2005: An experimental study on thermal circulation driven by horizontal differential heating, Journal of Fluid Mechanics, in press. ' i7 H! g& Y( M( Q! D# {, G/ R$ ]' `, ^2 x; n% J; o) X Huang R. X. and X.-Z. Jin, Gravitational potential energy balance for the thermal circulation in a model ocean, manuscript submitted to J. Phys.Ocanogr.6 @/ q* F; z2 s" v0 B2 { " W$ b; p1 V, K# J5 g Huang, R. X., W. Wang, L. L. Liu, decadal variability of wind energy input to the world ocean, manuscript, submitted to Deep Sea Research II. & A' M1 N8 B0 V) `. v' V 6 a1 Y- q' U/ X3 F- C7 v7 {6 P 5 S" k$ @# u( P4 B4 jNon-Refereed Publications5 d" F! L Z2 A! e9 B 8 i1 f2 G7 v$ b) U& R/ }0 s6 u Huang, R. X., 1976. Some problems in the supersonic stream—surface theory.   Information of Mechanics, No. 2 (in Chinese). ; K4 K* j# ], \& t* |# o ! A9 \, h2 D2 i. X( nHuang, R. X., 1977. On the stream--surface theory. Information of Mechanics, No. 1 (in Chinese). " Q4 z$ ^" H0 y, |- D/ r4 J3 f9 B/ \$ N1 t1 H/ Y3 z( @ Huang, R. X. and J. A. Wang, 1977. The Earth's mantle convection, a problem in geophysical fluid dynamics.   Information of Mechanics, No. 3 (in Chinese).8 U, P4 D$ Q: Q+ R) q9 ? + p2 |( i# ]; @, ` Huang, R. X., 1980. On the one--dimensional approximation of viscous fluid flow. Progress in Mechanics, No. 3 (in Chinese).3 Y9 ~5 N, U- q( Z7 |2 v; z2 ~ }0 P+ K4 M/ _2 w# _! rHuang, R. X., 1992. Deep western boundary currents. Oceanus, 35, (2), 26-27. 3 s' `( ]: K' s% g# A6 G6 p G7 F$ r( V O6 IHuang, R. X., 1992. Freshwater driving forces---A new look at an old theory.   Oceanus, 35, (2), 36-37. & b- X, O7 b" p6 l9 h6 y9 \$ c & F' H- a u/ @3 L% k9 l jHuang, R. X., 1992. A trip to the MBL Library with Hank. Oceanus, 35, (Special Issue: A Tribute to Henry Stommel), p. 126. 6 N: o! q8 I; n! i# z+ n+ B3 @4 g 5 X S, F1 I$ o! C8 x8 `, W7 {Hogg, N. G. and R. X. Huang (editors), 1996. Collected Works of Henry M. Stommel (3 volumes, 1943 pp), American Meteorological Society.# Q* W6 ~! g' l5 B5 D 2 ]9 i0 y( @' w& G& \9 T, b% lHuang, R. X. and J. Yang, 1996. Oceanic Aspects of the Climate Modeling, Oceanus, 39, (2), 36-38. 0 ~+ ^! J" `/ J- y9 M: {( g# n % `" H/ i/ o ^' |Huang, R. X., 1998. The future of physical oceanography, a personal view. A speech at the NSF-sponsored Physical Oceanography Workshop. * p2 e! x" p# l8 `0 q w% A* z; a+ c! u/ O' z Huang, R. X. and W. Wang, 2003. Gravitational potential energy sinks in the oceans. Near-boundary processes and their parameterization, Proceedings, Hawaii winter workshop, pp239-247. 7 X/ S5 E$ I& j2 I# u1 x3 k2 x) L7 u6 P W. Wang and R. X. Huang, 2004: Wind energy input to the surface waves and Ekman layer, Bull. Amer. Meteo. Soc., 85, 818-819. ' p- _% T8 `2 K% o / _. M( h" O2 X3 S! E' ]3 z5 w6 lTechnical Report & @, i; i: e V' f( N6 G% |0 v5 v: [/ `( ?, ~ Huang, R. X., 1983. A two--layer model of the subpolar gyre and subtropical gyre. In: Summer Study Program in Geophysical Fluid Dynamics, Woods Hole Oceanographic Institution - ?. z: O/ T3 E/ I p Technical Report WHOI--83--41, 106. ! W" m, r4 J& x* m$ W M5 m4 u2 ?) f - `1 } T. C3 |$ kContributor to Chapter 5: Climate Models-Evaluation in "Climate Change 1995", The Intergovernmental Panel on Climate Change, World Meteorological Organization / United Nations Environment Program, 1996.. j! h: `9 ^4 s" R8 J# @9 y; z4 o- ] 1 y, u" b1 X7 O% @: V0 C2 e Book Reviews : u% z, N' y; X0 }2 v! L9 X- _/ v& \ Huang, R. X., 1987. Advanced Physical Oceanographic Numerical Modelling, James J. O'Brien, editor, D. Reidel Publishing Company, Dordrecht, 1986, 608 pp. Bulletin American Meteorological Society, 68, (8), 1032--1033.' `1 t- H% e6 R+ S U. J9 o " ~4 ^# T% \' E2 C( A: rHuang, R. X., 1988. Numerical Modelling: Application to Marine Systems, J. Noye, editor, Elsevier Science Publishers B.V., Amsterdam, 1987, 295 pp. Bulletin American Meteorological Society, 69, (7), 775. ) B- W* Y1 q( }1 w- a% s' g6 a. P2 J Huang, R. X., 1997. Review of Introduction to Physical Oceanography by George Mellor. American Journal of Physics.4 s. x/ f4 \1 ^ 0 A: ~! [! E5 M3 HThesis- q' D1 [7 P T z) @ ! p* l) T; K& ]$ k% v) [7 C Huang, R. X., 1984. The thermocline and current structure in subtropical/ subpolar basins. Ph.D. Thesis, Massachusetts Institute of Technology/Woods Hole Oceanographic Institution, 218 p., F- c3 l) s1 ^ 6 m% N$ o+ s7 W- c7 o0 y6 t c( FLecture Notes 5 m3 w1 p8 Y. n3 j; O3 ^6 W' } ( [; v+ l& K D! k9 @% q0 {Huang, R. X., 1988. Steady Circulation of the Oceans and Atmosphere. Lecture notes for M.I.T./W.H.O.I. Joint Program Course, 215 pp. : s9 J% V% E* r9 F! i( @- ~5 j9 I) r- m4 ]. m( e Huang, R. X., 1992. Recent Advances in Large-Scale Ocean Circulation Theory. Notes for lectures presented at the Second Institute of Oceanography, Hangzhou, China, October 7--17, 1992, 237 pp., published in China. 3 A8 H2 L: I$ h / a: k) d$ h* n* g$ L+ [$ sHuang, R. X., 1995. Advances in Theories of Wind-Driven and Thermohaline Circulation, Tech. Rept, JIMAR-95-1, Joint Institute of Marine and Atmospheric Research, Honolulu, Hawaii, 211 pp. ) ?2 e) k2 {6 r/ E: c* ` : X% }# t. c- t* x* k: {- bHuang, R. X., 2004. Theories of the general circulation in the oceans. Lecture Notes for M.I.T./W.H.O.I. Joint Program Course, 600 pp. 3 P4 ~3 m) i7 H & O) n: v" n3 Z/ BReference Book. L! Q3 u+ H! w : \) V. ^1 }( z$ q; `Wang, T. Y. (Chief Editor), R. X. Huang, et al., 1980. English--German--French--Russian--Chinese Dictionary in Physics, Atomic Energy Press, Beijing, China, 2012 pp.
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