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师资介绍 黄瑞新教授

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黄瑞新教授 $ x& ?% \ b( F3 u( j" Y$ p 5 b3 O: T. t! o: `/ Q3 K* p ( m4 q7 H; r; H1 a, |" s- z' b' X Rui Xin Huang * \1 t6 q! y# H; O/ h2 Q( _# y) N( w8 j+ P/ F Senior Scientist9 q) C4 P4 T0 l! d2 V! I7 ] W. Van Alan Clark, Jr., Chair for Excellence in Oceanography, 2002-; 6 E( a7 \+ p6 t2 T% U) D4 E; M; \ D2 {Woods Hole Oceanographic Institution0 m/ L* m) ^! r: z + E7 q4 J6 |' @4 b% ]* oPhone: (o) 508-289-2532; v6 i- X! G5 `: ~4 \, j3 [% Z# ^ FAX: 508-457-2181; % E& J& a4 A7 @2 v u e-mail address: rhuang@whoi.edu 3 h5 e6 W2 Z, s6 [; D$ ZDate of Birth: Sep. 15, 1942 4 {( I' p" X0 HCitizenship: U.S.A.# y! u7 P) z! W( x* X2 N 1 Z% C4 K8 p; r% p3 @ Education" @* z3 e3 E$ P+ S . C3 y8 g, B4 t3 o @) x" s The University of Science and Technology of China, 1960-65; B.S. in4 x3 i$ ?* m! O Thermo-physical Fluid Dynamics of Jet Propulsion, 1965. 0 k& I. w$ j8 ]1 ]% ]" w2 H, t* A) |. v$ |' u Graduate School, University of Science and Technology of China, Meteorology, 1978-80.' }+ y) h* z: I7 E, N! B ( y2 ~# o0 }0 k) k The Johns Hopkins University, Geophysical Fluid Dynamics, Sep. 1980-Feb. 1981. 7 ]; V8 a6 t! u6 B4 E/ D 7 F4 ?+ }! x; F- f5 F( `' R9 kMassachusetts Institute of Technology/Woods Hole Oceanographic Institution, 1981-1984; Ph.D. in Physical Oceanography 1984. ' M6 E( Y) D* C ( p$ \. U6 U0 ~7 rExperience& W3 U# r& U2 w. _% S , I8 [, I3 T) X, O2 V6 E- j Research Associate, Institution of Mechanics, Beijing, China, 0 {' C7 U% m2 E W+ Z* s* ? & L4 [4 J, @9 v, S# H/ U& o1965--1978. Self-study of English and mathematics during the # t. D0 ~6 b5 K9 W) ~9 f' E4 sCultural Revolution in China; aerodynamics of wings; transonic flow in x; c- w$ [2 j$ a* b+ J 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.1 u" y1 s# s/ |( E2 i2 \ 8 ?( {; _. K. P% gPostdoctoral, M.I.T., 1984. * Z7 l; Y5 L8 K7 G: ]$ b4 S, dVisiting Scientist, Geophysical Fluid Dynamics Laboratory (NOAA), Princeton University, 1984--1986, March--June 1992.9 j/ {( U3 P& g/ m) V) ]5 e) K 0 v$ J# s7 J( i$ ^0 B# E- a8 n2 e" | Assistant Scientist, 1986--1990; Associate Scientist, 1990-1998; tenure awarded, 1993, Senior Scientist, 1998-, Woods Hole Oceanographic Institution; # r( ^9 i. Y5 J' y3 b , j. O/ D L9 ?, G0 j9 D9 O. N/ R/ eVisiting Associate Professor, University of Hawaii, Jan.-June, 1994.$ a( i. ]$ q( {$ c1 t9 x, u 9 o3 g" P' [4 j# r6 ?6 ` Visiting Scientist, Cooperative Institute for Marine and Atmospheric Studies, 7 V M. ` y; BUniversity of Miami, Feb., 1999.- j( D: ]3 P# e# w- n8 L8 F7 E & p5 i+ n( d/ G3 @9 V8 {! g# u Visiting Professor, Lamont-Doherty Earth Observatory, Columbia University, March-May., 1999. ) Q- V8 E: O6 p+ S& L! F$ L0 k9 Q. Y7 _6 O5 F Corresponding Member, U.S. WOCE Working Group on Numerical Modeling, 1989-1992.1 S( E8 D: ]. l% d0 V: L 9 q, `% Q2 q; l1 e3 dJoint Committee of Physical Oceanography, MIT/WHOI Joint Program, 1990-93.9 G( Q, ~4 r* K # Y3 c1 ?( l9 m" n; G W Member, Working Group on Oceanic Thermohaline Circulation and Variability, 4 X- q* D- B( OClimate System Modeling Project, USA, 1993-96.% N, g8 f- |7 F9 Y$ o. ?" f & ^8 B( s* [# C( I7 n4 ]Member, Climate Change Committee, WHOI, 1995-1999. " C# V! v; [- I( e/ k! j9 Z: N+ H0 k R Member, Advisory Committee, Ocean and Climate Change Institute, 2001-2005. $ M. O5 S* O. |* j ~9 V ' G0 |- W# j6 Q5 eGuest Professor, Ocean University of Qingdao, China, 1996--. $ w# H1 I8 z" |3 C8 X! z5 d, y 3 f# } N, g* o5 z0 `4 n3 _Chairman, Academic Committee for the national Key Laboratory of Physical Oceanography, Ocean University of China, 1999-2005.( Z: k/ K( |0 k" u; S ' O/ z3 |2 W% V1 V6 e# q( d7 j$ C Member, 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. ! w9 B7 V8 _2 ?$ I) V 9 e7 v3 ` @) p9 e7 Z( @3 f* JGuest professor, South China Institute of Oceanology, Chinese Academy of Sciences, 2002-.; {: j7 i. q0 I* ] * a. t* A7 P8 Y, Q/ B # _( r7 r& B, e, C* B- W Teaching + t0 N* K7 x4 D# \- a( ? L! y2 h' | t% HSteady Circulation in the Oceans and Atmosphere, MIT/WHOI Joint Program, 1988-1991.2 g7 u0 z% f7 j/ D1 |) C' W + C. ]8 w; I1 o" ?4 k& r; iRecent Advances in Large-Scale Ocean Circulation Theory, Second Institute of Oceanography, Hangzhou, China, October 7-17, 1992. # T: p( J3 F( E, h9 O0 e, ]8 u9 K/ t- b8 [" O( Q; { Theories of the Oceanic General Circulation, University of Hawaii, Spring, 1994.7 x/ O/ t2 q y- r ) m3 r* i# x& Q- t" |Advances in Theories of Wind-Driven and Thermohaline Circulation, International+ l7 ^: ?2 v" }$ K5 g- w % Q% b1 r B: U* a( l) tSummer School on Ocean-Atmosphere Interaction, July 25-August 4, 1994, Qingdao, China.8 q+ @) G" M% \ ' j* H& h& P: s; c9 N% r Theories of the Oceanic General Circulation, MIT/WHOI Joint Program, ) n& X6 R1 p4 z/ }. j l9 ]: H: P( q" U: `4 s Spring 1995, Fall, 1998, Fall, 2001, Spring, 2004. % u3 m6 V0 v6 R: w8 g7 ] f1 G3 D3 P6 ? Supervision & H$ m. ?( A/ M# y3 C( b( d$ W( m& Y# z- W' @% T! o. G 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).7 a4 ]3 [( p- Q* O; t$ o7 h, i 4 ]; n$ d; P& W8 N Mr. James McLaren, 1987-89; Mr. Li Ping Wang, 1989-93 (Ph.D.); * o1 f1 m. f3 W: N( [" i . s" L% ^, |6 F0 V% e FOn thesis committee of other six students, chairman of thesis defense committee for Mr. Hui Ming Zhang and Ms. Sarah Gille. ' {* ?% E% m0 A- ^3 E! q+ e& ^ ! k7 `# f. c( K) s2 U" a; xMichael Masterson, Summer Student Fellow, 1987; Marcel Lieberman, Summer Student * ?0 b/ M& p) i" w; C2 C1 E8 @Fellow, 1989; Sarah Russell, Summer Student Fellow, 1993. . l# \$ a- a% ` ( {! U" p" T+ {# Q2 m; [2 J- }1 M( `Sea Cruises 9 i. ]. g% E/ t ^1 H: f$ q ; P8 Z L1 u4 S' T* h/ x- I+ |2 WRV OCEANUS, Seasor test cruise, July, 1989. % i: O* Y9 r& |& ?4 A% rOceanus, Immerges Sea Cruise, August, 2003. $ N$ g( v5 K% a( x7 G+ O: o ' ^- H& O4 r n g4 {# Y Honor7 {+ X7 F- n6 ~4 T - f! d+ B' P; b* C4 dNominee of President Young Investigator Award, 1989. 0 c, U) n+ q* m5 ?1 g+ F I0 P, w) w Research Interest:/ X) }$ I( ?9 c7 d ! y* @9 h5 ?) @) w/ T- s& ]! jTheoretical 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. - Q b( e9 {- L3 ]% a) ~" ?& t5 E / c6 t* M4 K% ?) v$ l( XAuthor or co-author of 70 refereed scientific publications. 2 G& A6 Z# J% u/ ~) J/ i% q: E* N4 | Refereed Publications % ?; v' R! e' g v & @1 o, X) h# k$ }% PHuang, 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). 0 T/ T2 @! q1 {8 S( ?+ p( Z8 z! S+ r Chao, J. P. and R. X. Huang, 1980. The cnoidal waves of a rotating barotropic atmosphere.   Scientia Sinica, XXIII , No. 10, 1266--1277. & H0 X6 f, P# a2 g/ _, [; ?2 {6 C, P5 |2 q( J Huang, R. X., 1986. Solutions of the ideal fluid thermocline with continuous stratification.   J. Phys. Oceanogr., 16, 39--59. ' _7 }( ~ [! v0 I, R; b% K' R4 ^ Bogue, N. M., R. X. Huang, and K. Bryan, 1986. Verification experiments with an isopycnal coordinate ocean model. J. Phys. Oceanogr., 16, 985--990.0 A5 ?; x6 l1 _- ? & `& x$ b3 l! U. K6 _0 S Huang, R. X., 1986. Numerical simulation of wind-driven circulation in a subtropical-subpolar basin. J. Phys. Oceanogr., 16, 1636--1650. 4 X" e2 z& k8 t) [* V ; ^) `$ E) \9 T8 K" j5 x/ s6 BHuang, 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. / F* p0 i! N4 @! v. z$ N! V8 x# a/ S; @8 F$ O Huang, 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. ! i" r, H e4 l4 J7 m7 X+ z , x7 ?4 U: q0 x* G+ bHuang, 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.- j1 |3 @" f2 N3 p+ H 9 \' ?" ~& `5 W5 C. O7 N 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. ( B2 }# P! |8 J) ?) Z# @+ u) r3 a3 b- z/ y# J Huang, R. X., 1988. On boundary value problems of the ideal-fluid thermocline.   J. Phys. Oceanogr., 18, 619--641.3 U w4 @ q& e# W! K 7 q( Z/ k0 I6 b3 [; Y$ OHuang, R. X., 1988. Ideal-fluid thermocline with weakly convective adjustment in a subpolar basin. J. Phys. Oceanogr., 18, 642--651. 9 l) _) h9 B) a1 Y & |) P- R# w. k1 f5 C; x; x+ }' jHuang, 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--752.8 C' A( i" ]5 D* s+ O( V 8 O. B3 q5 f# U- d2 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. 5 N( l, ]4 |$ l$ }' Q9 H( _( u/ _# Y9 {. E |$ J) V9 {8 h Huang, R. X., 1989. Simulating the main thermocline in the North Atlantic with an ideal-fluid model.   J. Phys. Oceanogr., 19, 543--547. 8 L' K4 T" h9 g3 ?* I% g8 u& R; s. J$ [/ k, V 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. 9 A0 L8 h) H; o' r( g3 s. Z# w. w$ U1 |9 C3 m- a4 S8 f Huang, R. X., 1990. Does atmospheric cooling drive the Gulf Stream recirculation?   J. Phys. Oceanogr., 20, 750--757.6 H/ R. l" E" E/ g5 [$ ? 6 ~, K8 i+ J3 C) n" o: `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--159.7 J3 w. t7 }6 \8 O4 A; }1 z! S : ^/ F3 X+ ^# [, [( r' m: _* YHuang, R. X., 1990. On the structure of inertial western boundary currents with two moving layers.   Tellus, 42A, 594--604. ; o0 z) f% M# s8 _# r! i0 [ ' Z, I7 L6 ?! ]" I+ k) X- QHuang, R. X. and H. M. Stommel, 1990. Cross-sections of two-layer inertial Gulf Stream.   J. Phys. Oceanogr., 20, 907--911. + N: `4 `9 ?0 ^( e2 C- b0 @8 x4 H. u5 A9 y f( w, ]2 Z2 a Huang, R. X., 1990. Matching a ventilated thermocline model with inertial western boundary currents.   J. Phys. Oceanogr., 20, 1599--1607. # t O8 x9 H& n8 W% W* K % S% C3 D* j; [& F% K i, cHuang, 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. # e, _1 o4 U# r8 _: z3 D( h1 }& }; t9 Y: D& t$ B \! k4 \ Huang, 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. & v# G/ f( D/ C9 m # Q+ @0 v, } b I0 ?Huang, R. X., J. Luyten, and H. M. Stommel, 1992. Multiple equilibrium states in combined thermal and saline circulation. J. Phys. Oceanogr., 22, 231--246.# A# u" g/ d& K+ `) C7 \& `6 [ 2 k) I8 X, q5 M' c! z Huang, 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. ) V1 E4 K: o6 V$ x: y* c Z, u& j, V# j( O1 {; a) Z 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--10,036.7 k$ {" X7 W3 u- W, `# O 2 V8 x% c- _3 i( dHuang, R. X., 1993. A two-layer model for the wind and buoyancy forced circulation. J. Phys. Oceanogr., 23, 104--115. 5 i% m7 X% c$ r* C$ h. m+ d+ f( h0 p6 u Huang, R. X. and R. W. Schmitt, 1993. The Goldsbrough—Stommel circulation of the world oceans.   J. Phys. Oceanogr., 23, 1277--1284. 2 v$ `7 @/ ^$ ^3 B2 q% t! |. n2 l- h9 \( K Huang, 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. " {0 n* ^( U% n2 R1 R 8 E0 b# X" I! o2 R0 M5 }* fHuang, 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), 181-184.0 b( h4 ^- G) | 4 v8 j. B! }9 R) @4 \ r Huang, R. X. and R. L. Chou, 1994. Parameter sensitivity study of the saline circulation. Climate Dynamics, 9, 391-409. 4 L& X' c5 N- G( v$ I* Y+ h/ I3 ]+ O3 t- [7 b* e' R" L3 u Huang, R. X., 1994. Thermohaline circulation: Energetics and variability in a single-hemisphere basin model. J. Geophs. Res., 99, (C6), 12,471-12,485. 0 h7 l6 H" w$ j- e0 _9 Q! d0 V& N1 |: Z( d 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.$ D z3 V3 g% U7 G! O& C) g9 l 8 O4 ] A- D( } Wang, L. P. and R. X. Huang, 1994. A simple model of abyssal circulation in a circumpolar ocean. J. Phys. Oceanogr., 24, 1040-1058.7 Q0 ?6 U) Y. J 2 f% x$ w# |% E Huang, R. X. and S. Russell, 1994. Ventilation of the subtropical North Pacific. J. Phys. Oceanogr., 24, 2589-2605. 7 @4 S6 S6 X. Q) b6 A8 A0 s' h( O/ ^8 h" Q+ | 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. , u9 i) [4 e/ J1 X C4 f1 I, y! i% C! y. Z* O2 {4 g3 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. * x! c6 u1 S4 `% v. i2 O2 O! ]/ H% }3 S. R, O; V Pickart, R. and R. X. Huang, 1995. Structure of an inertial deep western boundary current. Journal of Marine Research, 53, 739-770. : w1 E2 S# V) C& B" d! V % m8 U& h4 I% XQiu, B. and R. X. Huang, 1995. Ventilation of the North Atlantic and North Pacific: Subduction vs. Obduction. J. Phys. Oceanogr., 25, 2374-2390. : }5 @ u2 \ } E9 J# N0 ^* B ) m) k3 o2 I* j3 B+ Z: a4 {, D5 [Huang, R. X. and J. R. Luyten, 1996. Reply. J. Phys. Oceanogr., 26, 286. 0 Q; A. {( d* I8 f " l7 m+ e! ]6 m3 {& d6 B: TDewar, W. K. and R. X. Huang, 1996. On the forced flow of salty water in a loop. Physics of Fluids, 8, 954-970. & i4 g4 _5 Z1 R) \0 q: Y0 C O 4 u1 a$ W w$ W+ V9 E* d) s t; ZYang, 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, 269-272.5 t T7 Z; O* ^ d* D- k$ ~6 O 3 m9 W2 J8 C; b- E x* s- X7 ~5 QHuang, R. X. and W. K. Dewar, 1996. Haline circulation in a loop model: bifurcation and chaos.   J. Phys. Oceanogr., 26, 2093-2106. , ~5 w: ^7 F m" M: t5 E/ v9 j# _ q D2 ^( \) O( m: d8 c Huang, R. X. and J. Yang, 1996. Deep-water upwelling in the frictional western boundary layer. J. Phys. Oceanogr., 26, 2243-2250. 0 Q- h& l4 y! ^1 y- f5 J F# p Huang, R. X., 1998. Available potential energy in a Boussinesq ocean, J. Phys. Oceanogr., 28, 669-678. 6 Z2 ]$ F, [( V$ V7 s/ @2 l& X 9 E: C! f) a6 oHuang, R. X., 1998. On the energy balance of the oceanic general circulation.   Chinese Journal of Atmospheric Science, 22, 452-467.+ m( a: U. Y1 A, _8 U1 C' j/ m 2 Y/ Y0 I1 x8 M+ r- i/ EHuang, 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. 1 i8 R/ q8 d+ N6 |% W7 M" S " l2 O3 K: e. pWang, L. and R. X. Huang, 1998. A homogeneous model of the Decon cell in a circumpolar ocean. Dyn. Atmos. Oceans, 28, 157-177. - j. s2 J3 s* ^/ q' Q, U$ N2 T0 p q3 _/ b6 L1 ?$ D2 N Zhang, J., R. Schmitt, and R. X. Huang, 1998. Sensitivity of the GFDL Modular . L5 Y" e+ w$ [. L( A$ tOcean Model to parameterization of double-diffusive processes, J. Phys. Oceanogr., 28, 589-605. : |7 E! V L9 {/ D$ x* |% ]3 ^8 I8 }% o 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.( ]/ W" |. d0 w. ~ _: Q U @% x+ H6 G6 P% Z; ^) a% t Huang, R. X., 1999. Mixing and energetics of the thermohaline circulation.   J. Phys. Oceanogr., 28, 727-746. " a* M7 g4 N5 I1 l2 S7 l/ ?- J% T. s( n& j" k- v% W! q 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. $ M, _ ~5 t G! l. S2 j4 y$ v, ?- R+ Z; T 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.! L* m6 A% z7 d) i. e2 T* ?. s3 d $ ?/ s/ l9 F Z. R( f Huang, R. X. and J. Pedlosky, 1999. Climate variability inferred from a layered model of the ventilated thermocline, J. Phys. Oceanogr., 29, 779-790.! _8 M1 p' R0 [ 9 L1 G2 p4 R2 K0 H! b; r Huang, R. X., 2000. Climate variability inferred from a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 389-1406. + l" S z- D- _6 x% o0 S A 0 [* I% n& O; q- s% ]* V' Y I) l Huang, R. X., 2000. Parameter study of a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 1372-1388. {1 u" }% y; I" H/ `9 A, w. n " h& R& N3 V9 w8 r: k' {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. I+ N" R8 y1 P# l . [8 [' A) {3 _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. ; ^; d7 n9 x( _ 4 j4 z: ]5 O3 s- o |Huang, 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, 759-762.4 p6 D0 u- T) m$ _* n5 p# Z 6 s" o1 z- W7 EHuang, 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. 3 D8 R( ^7 n) C( l [% `3 | 8 m- V# O. }; n$ Y, q) V" }Huang, Rui Xin, 2001. An analytical solution of the ideal-fluid thermocline. J. Phys. Oceanogr., 31(8), Part 2, 2441-2457.% S; X7 o1 O* l+ Z x3 k) b$ f ' D b' t2 H) d6 [0 L, Q1 tDewar, W. K, and R. X. Huang, 2001. Adjustment of the ventilated thermocline. J. Phys. Oceanogr., 31, 1676-1697. 3 h0 w+ g$ v8 Y8 p3 G4 s2 o( z& L3 n! F% [0 h Huang, R. X., and Q. Wang, 2001: Interior communication from the subtropical to the tropical oceans. J. Phys. Oceanogr., 31, 3538-3550." N+ r( I* a, q( p) o , u- f! O- d& C8 q4 u6 @* }) |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. 5 n6 X2 \: ]" [- M# j& p ! V# d+ ?5 I1 d" K' Y3 B Huang, R. X. and J. Pedlosky, 2002. On aliasing Rossby waves induced by asynchronous time stepping. Ocean Modelling, 5, 65-76. ; }3 B/ }: i. U! B1 m5 P; k' k # _$ G" |& m% R6 K8 xHuang, 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. ! D" {/ U& K% W 9 j2 L9 C. m0 K, M" R& E1 t: E 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, 2131-2150.9 O" f" h# d/ F: d ( B& }- [2 w0 m- p4 BZhang, 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 K) a. S/ ^- d# g0 J 4 f+ X6 o* B7 g7 S# I2 SHuang, 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. " b, \! \) w9 _+ Q+ s 5 O1 ~, ]% G& X$ @& b# Y' gWang, W. and R. X. Huang, 2004. Wind energy input to the Ekman Layer. J. Phys. Oceanogr., 34, 1267-1275." `5 R: y" @7 q0 @, U. p 4 t& x, o- ]( x. A4 Z( } Wang, W. and R. X. Huang, 2004. Wind energy input to the surface waves. J. Phys. Oceanogr., 34, 1276-1280.4 K4 @! ?- k2 @- F ; C+ v( r9 X0 ]/ C7 r2 p: v; e5 YHuang, R. X., 2004. Ocean, energy flow in. C. J. Cleveland (Ed.) Encyclopedia of Energy, Elsevier, Vol. 4, pp 497-509. , c! }- I% L+ I& ^/ Q & E: j( n1 v- l( wHuang, R. X., 2005: Available Potential Energy in the World Oceans, J. Mar. Res., in press.# S1 @" i9 n- y* W % t/ F* U: r& p1 `9 M; e Wang, Q. and Rui Xin Huang, 2005: Decadal Variability of Pycnocline Flows from the Subtropical to the Equatorial Pacific, J. Phys.Ocanogr., in press. $ w& \5 ~9 S0 @9 |! u . r6 f1 P, L* \$ e: I% Z1 X9 hWang W. and R. X. Huang, 2005: An experimental study on thermal circulation driven by horizontal differential heating, Journal of Fluid Mechanics, in press. 8 y8 a2 ` y/ n7 i3 \( w( [# t. D 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. / z% r$ K1 U8 m8 g4 c |; ^, K) g0 a$ U6 tHuang, R. X., W. Wang, L. L. Liu, decadal variability of wind energy input to the world ocean, manuscript, submitted to Deep Sea Research II.3 f# k! i5 c q, z 8 q) p' d% P* T3 ~! R( A# V" {2 q$ s+ c1 W Non-Refereed Publications x2 q7 g. |- u: L+ _$ x, x2 o7 \5 X+ M1 {* ]- f$ Q Huang, R. X., 1976. Some problems in the supersonic stream—surface theory.   Information of Mechanics, No. 2 (in Chinese).0 m# D0 ]/ J1 f5 {1 e7 U 3 l8 w8 k+ `4 v2 h& @# W1 H2 THuang, R. X., 1977. On the stream--surface theory. Information of Mechanics, No. 1 (in Chinese). * U/ b3 U% v: t" ^ 8 V5 G& F4 @, U$ K( JHuang, 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). 3 E; Q' U# d5 `7 q) p4 f1 m/ {1 ?& R5 W + s' B6 T# T# `0 v: iHuang, R. X., 1980. On the one--dimensional approximation of viscous fluid flow. Progress in Mechanics, No. 3 (in Chinese).1 ^. J0 e5 G4 @1 [8 z: D3 E . e' y: k4 L/ B5 `Huang, R. X., 1992. Deep western boundary currents. Oceanus, 35, (2), 26-27. 5 u4 z4 x- B; w+ J8 n; o' T Q+ m: ~' o. m Huang, R. X., 1992. Freshwater driving forces---A new look at an old theory.   Oceanus, 35, (2), 36-37.4 i" F" P/ j' Y' a0 ? ) P8 ?5 j( f& \3 w3 ]* bHuang, R. X., 1992. A trip to the MBL Library with Hank. Oceanus, 35, (Special Issue: A Tribute to Henry Stommel), p. 126.0 G1 L, Z9 Z1 N9 J $ t9 t2 k. _9 e# M6 dHogg, N. G. and R. X. Huang (editors), 1996. Collected Works of Henry M. Stommel (3 volumes, 1943 pp), American Meteorological Society. * y/ Y+ V2 ]9 v + Q2 t) Z% g2 T$ F2 X6 mHuang, R. X. and J. Yang, 1996. Oceanic Aspects of the Climate Modeling, Oceanus, 39, (2), 36-38. 5 `* a- w; y4 P a4 k! x# [" Q! j# w0 u Huang, R. X., 1998. The future of physical oceanography, a personal view. A speech at the NSF-sponsored Physical Oceanography Workshop.. u) J% _8 a& T/ @, m+ C6 U7 V 5 k6 S4 J* w7 a- T2 i/ X1 y2 m2 Y 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. # {0 M, Q' }0 e6 s # {0 E6 J3 \/ b E6 i! yW. Wang and R. X. Huang, 2004: Wind energy input to the surface waves and Ekman layer, Bull. Amer. Meteo. Soc., 85, 818-819. / Y$ P# Y/ U1 M1 D \ 5 t, A; }( k5 NTechnical Report1 Z1 n' W! s' ^- ^- T 4 ]* f! @* s; f; c& ~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 % E/ k& Q6 b. t# }( r- F& O/ S Technical Report WHOI--83--41, 106. ( a& d7 P$ S' V1 a n" o & G; G6 D8 m. Y- R0 w, qContributor to Chapter 5: Climate Models-Evaluation in "Climate Change 1995", The Intergovernmental Panel on Climate Change, World Meteorological Organization / United Nations Environment Program, 1996. / H0 Z. K, j" R, Z$ g# X& w7 b$ S$ e F" X Book Reviews/ ]) e4 F( b; ^4 w ' H( q" l/ y( F5 v5 k5 WHuang, 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. 0 [+ P" x' X0 n" S p P# I6 ?7 H" P$ t, h Huang, 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. 8 `% M! N4 r$ z Y; M9 {$ n2 ^" c7 n( A Huang, R. X., 1997. Review of Introduction to Physical Oceanography by George Mellor. American Journal of Physics. ' n( T$ i; g6 w1 R( g( q 9 }' v9 f" k6 A5 y {! }) u6 rThesis ) l# g) b2 j3 N1 S( w9 z+ h" w( ^: |2 K 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.0 e1 @' [5 B9 Z; P ! ^. V+ J! e+ G3 TLecture Notes ' q6 D8 T( f7 n8 {9 ` : O2 K+ `; ~9 D6 Y9 q. ? iHuang, 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. + x0 i: G4 O* K$ Q* ^: _, f4 L- K$ N: F! G3 m ^! r# ~ 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. / ~% S2 B- H+ u( n! E1 \8 N : l! k$ K& Y! x7 i. zHuang, 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. 4 Q9 e H0 F" p4 e, q4 T * @2 q6 Q7 c) J4 l" a: Z: p; l4 }+ aHuang, 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. 5 Y5 `+ R! g; E. E# k' k" ^$ m) n. r; {; O% z Reference Book+ p. y# O+ g, D) d! M# | ) D: d) s8 l5 k! J ~0 w 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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