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师资介绍 黄瑞新教授

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黄瑞新教授 ! u; [% b5 Y9 r) @/ z, I" i / y# Y! s; P! C! Z2 w$ B: U3 b. l% o& O( z; L2 [2 ~ Rui Xin Huang % ^+ K/ e0 k0 R w5 @' ~4 n8 f4 Q9 V7 n Senior Scientist + F+ o( T0 x6 @4 iW. Van Alan Clark, Jr., Chair for Excellence in Oceanography, 2002-; - e5 ]5 P3 n' ~3 a% X* z* q* [Woods Hole Oceanographic Institution ) E ~. R: _* ^5 I ' [" Q6 D; Q* E; W8 PPhone: (o) 508-289-2532; 3 | W- W( o1 |- k9 kFAX: 508-457-2181; 0 ^0 j& U& q; h3 F/ X/ Z e-mail address: rhuang@whoi.edu/ a C9 T; ^; v) r Date of Birth: Sep. 15, 19423 ]& h" _2 {- }- f9 _$ G, T Citizenship: U.S.A. ' X; t0 n6 x8 m7 \8 m) ] 6 m4 ]* G& Q% I2 t; ?4 Q" I) QEducation2 B7 Y7 d' j3 {9 O5 w ( ^) D; m! d; {. A0 M$ I: i4 I& eThe University of Science and Technology of China, 1960-65; B.S. in & D# L% @0 C; G( u2 m" _Thermo-physical Fluid Dynamics of Jet Propulsion, 1965. ( J+ g: X- K$ X4 \ 1 @5 S* O8 _( ]% Y' |7 L7 X# cGraduate School, University of Science and Technology of China, Meteorology, 1978-80.0 X! O3 @: w6 G" m" R( } 2 j% M% I( d7 W* R" S# a$ |# a9 rThe Johns Hopkins University, Geophysical Fluid Dynamics, Sep. 1980-Feb. 1981. & @% k2 f% e3 C) H ; J/ t/ _/ p+ k: l8 h/ xMassachusetts Institute of Technology/Woods Hole Oceanographic Institution, 1981-1984; Ph.D. in Physical Oceanography 1984. 3 x& p" W2 e* M3 ]5 K/ p* H, ~ * B1 W: n/ f, M' M% U* H! ]9 p Experience - e9 r$ K% `& @* A( Q q6 r3 F' l4 h7 l+ B3 b k1 c1 [ Research Associate, Institution of Mechanics, Beijing, China, ; J! {. j8 p4 r$ K: s' Q2 H 0 P7 z% C) }- Q; B3 z1965--1978. Self-study of English and mathematics during the . [8 U1 b* k; \, E4 p z Cultural Revolution in China; aerodynamics of wings; transonic flow in - A& [$ ^" o8 [0 u' V% H; x! lTurbo-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.' v0 B5 A0 i( k , u. C- |) f: @ a Postdoctoral, M.I.T., 1984. 7 T1 H6 w% j# L9 P Visiting Scientist, Geophysical Fluid Dynamics Laboratory (NOAA), Princeton University, 1984--1986, March--June 1992. M# I8 o+ B) V" ^3 \$ I* @3 r" K* {3 O Assistant Scientist, 1986--1990; Associate Scientist, 1990-1998; tenure awarded, 1993, Senior Scientist, 1998-, Woods Hole Oceanographic Institution; 2 [4 N( M2 S8 k+ Z$ |1 q3 Q; z6 b" \( |# [7 N* `5 D Visiting Associate Professor, University of Hawaii, Jan.-June, 1994. $ ^; @' S' x, T3 p8 X0 r ; `; P o/ v6 d! c+ x; v5 OVisiting Scientist, Cooperative Institute for Marine and Atmospheric Studies, , c4 |( M; T8 s; T7 z6 |University of Miami, Feb., 1999. ; i# I) ^# Q- _& x* r* Q& V8 Y; r$ r* |; E6 j" I. ` Visiting Professor, Lamont-Doherty Earth Observatory, Columbia University, March-May., 1999. R9 P; k: ?$ {. w9 O( @ # n9 s; T1 b; I7 ~Corresponding Member, U.S. WOCE Working Group on Numerical Modeling, 1989-1992.* F+ J. @4 `( K' H- ? ; i6 F) \5 [9 Z3 S/ d/ GJoint Committee of Physical Oceanography, MIT/WHOI Joint Program, 1990-93.# J4 m+ Z1 `8 ]' n " u2 J( k" O* i* G! @) }Member, Working Group on Oceanic Thermohaline Circulation and Variability, 1 j2 \" X4 u% W, p- Q4 LClimate System Modeling Project, USA, 1993-96. 6 M! ^; N" P X& `8 G* w" V- g5 x4 G, y Member, Climate Change Committee, WHOI, 1995-1999., }6 h' ^- ?& r. T2 P7 j # c& U6 K1 W( x$ qMember, Advisory Committee, Ocean and Climate Change Institute, 2001-2005.- m' ? X3 `# [+ s ]& L. f* E V+ P, p( |' E% OGuest Professor, Ocean University of Qingdao, China, 1996--., f- G) [& |3 Z , {. w+ g! a( n2 t1 K- G3 r Chairman, Academic Committee for the national Key Laboratory of Physical Oceanography, Ocean University of China, 1999-2005.' F: [2 A6 ^+ e0 f9 F2 @ k1 t9 z, I5 T) q% U% u3 TMember, 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.) h7 v1 E9 C) R: r* W% h : ?4 k) v* Q8 |5 T1 n0 K7 r: ^; rGuest professor, South China Institute of Oceanology, Chinese Academy of Sciences, 2002-. 3 o0 X( S; T7 E- r 2 ^6 E; ^$ v& f; h4 T& I' ~, K& W7 z Teaching$ X4 {# I m" k$ @6 N6 @- b ) w1 f) n& P; M7 K. J5 m+ y Steady Circulation in the Oceans and Atmosphere, MIT/WHOI Joint Program, 1988-1991.+ f( a& L8 X0 x: L) X V1 D2 e4 h( c 8 s, I8 h/ L* b2 C% _! i$ d Recent Advances in Large-Scale Ocean Circulation Theory, Second Institute of Oceanography, Hangzhou, China, October 7-17, 1992. * k# z; m- p! Z. q: V 7 }# r1 |) [! Y- G2 Y9 I! XTheories of the Oceanic General Circulation, University of Hawaii, Spring, 1994.5 `, M2 L8 O" z% ~- o6 T0 a 1 j% y6 q6 N( l3 R Advances in Theories of Wind-Driven and Thermohaline Circulation, International' i6 [: x T/ }. Z/ J / K& E/ r2 d: s( K' C. c2 a Summer School on Ocean-Atmosphere Interaction, July 25-August 4, 1994, Qingdao, China.1 A& ?: j l- Y0 S4 k0 g) d# u6 z % p6 D6 Q6 u! R' Y7 p" P Theories of the Oceanic General Circulation, MIT/WHOI Joint Program, 0 O: t' S6 b' {/ E/ [ 4 ]* z& K: L- e- Q MSpring 1995, Fall, 1998, Fall, 2001, Spring, 2004.8 r8 E' P8 d& z* {* M$ S, I( I$ s 6 r, ?3 F7 N& h2 P: t) a" I3 G Supervision 4 L% `4 f2 k& r0 _' K $ K1 k' e) l% r3 FServed 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).8 `! B" E4 j% B8 W2 l! Q; E ) X; o# T3 e% @+ @3 } Mr. James McLaren, 1987-89; Mr. Li Ping Wang, 1989-93 (Ph.D.); ) A" d2 A) P9 O8 e! M0 H , T$ P) [* m2 u9 G# w5 eOn thesis committee of other six students, chairman of thesis defense committee for Mr. Hui Ming Zhang and Ms. Sarah Gille.3 R9 K. L8 R6 t% Q- b' a" _+ s 7 z. H/ D; \, r; tMichael Masterson, Summer Student Fellow, 1987; Marcel Lieberman, Summer Student* {, e+ b% c, f- j' T- k) o Fellow, 1989; Sarah Russell, Summer Student Fellow, 1993., T6 ]; S( F: P7 ^4 G" n8 ?, y z; v' S- j8 J0 }5 c1 vSea Cruises- ?5 _1 n4 l# q/ i- U/ k . W& o# b; ]& o+ d" o+ R RV OCEANUS, Seasor test cruise, July, 1989. 4 c; i" `* z6 y4 V( u9 n8 _. D$ uOceanus, Immerges Sea Cruise, August, 2003. 0 U2 P# X3 ~0 G% ] 4 N" e6 y5 x1 S- U+ AHonor h: Z. O( T9 [& p9 o3 y5 X* q8 J) L# |+ _0 V3 C6 ~% t3 j+ F- {6 S Nominee of President Young Investigator Award, 1989. 6 W; A! w. e8 }& E& ^, @ p, j( g( ^. K $ L$ G5 W& n" @# K0 x X: s: QResearch Interest: ( E4 U2 ^; o7 K& ^: r ]) A; D 3 M a' z s6 S5 s8 l- T" f9 k4 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.- y( |: L% V: ^# O 9 Y/ q* ^; x+ \3 a. A" a) T [7 C Author or co-author of 70 refereed scientific publications.& y9 X" Q6 m9 e- m/ L* l1 Q4 ^ ! \% {( U t2 _Refereed Publications0 q. o/ g$ m m. x. Q/ {7 M 6 x# b# R. u) V; W 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). 3 S% |6 ]6 t+ @# a( m ^# s ) z. [9 {. Q1 U2 bChao, J. P. and R. X. Huang, 1980. The cnoidal waves of a rotating barotropic atmosphere.   Scientia Sinica, XXIII , No. 10, 1266--1277., e6 k. S* u; u& f& e 5 E; n1 W3 B! E* |% g) H Huang, R. X., 1986. Solutions of the ideal fluid thermocline with continuous stratification.   J. Phys. Oceanogr., 16, 39--59.4 z# t: k! P* ^" p: P ) W5 o, ?& L5 |! [; y9 R Bogue, N. M., R. X. Huang, and K. Bryan, 1986. Verification experiments with an isopycnal coordinate ocean model. J. Phys. Oceanogr., 16, 985--990. 2 Q" d/ G2 p0 v0 }5 T3 p! n ; N3 f7 {3 j5 ?& q" x8 oHuang, R. X., 1986. Numerical simulation of wind-driven circulation in a subtropical-subpolar basin. J. Phys. Oceanogr., 16, 1636--1650. . M1 j0 ~5 e( y2 T" x: H9 u6 x 9 d, b7 i6 l& p% N6 u2 GHuang, 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.! S4 S! N4 @, D) D+ T 3 i8 c; d9 r8 d4 a, T2 I" e6 S 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. 2 A" Y0 p/ w# P4 C! A. @% @2 \9 p$ U6 K! |9 [4 u9 U 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.% c9 y$ t4 N4 [/ G % x3 \& R% V! @' K- z; g0 R) o 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 F( `' S+ T5 Y" \( N' M" L2 Q' {* }; m Huang, R. X., 1988. On boundary value problems of the ideal-fluid thermocline.   J. Phys. Oceanogr., 18, 619--641." F1 b) y3 L) y5 a0 Q & S) _" N& {" O Huang, R. X., 1988. Ideal-fluid thermocline with weakly convective adjustment in a subpolar basin. J. Phys. Oceanogr., 18, 642--651.& R0 g' _2 k8 L) P4 D) D/ h ! i4 K$ h% a! o! y* q7 x- l Huang, 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--752.7 _. C) N1 ^5 H2 a 1 E7 Z3 b/ K, E$ ]# OHuang, R. X., 1989. The generalized eastern boundary conditions and the three-dimensional structure of the ideal fluid thermocline. J. Geophs. Res., 94(C4), 4855--4865.2 J+ i4 Y4 j/ c( K% w% K0 U& v & H, G' ?* y4 U2 y" JHuang, R. X., 1989. Simulating the main thermocline in the North Atlantic with an ideal-fluid model.   J. Phys. Oceanogr., 19, 543--547.% ?. L& Y* p7 o, E _9 F 7 ~2 F2 V% G5 L d 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--18,021.2 n1 F. @% _% M4 z9 D L9 t1 Z# t8 n& ?8 i& EHuang, R. X., 1990. Does atmospheric cooling drive the Gulf Stream recirculation?   J. Phys. Oceanogr., 20, 750--757.9 \$ s. W3 o0 O" K% N& S! R) ~ \9 w: R/ X m, z* Z) x6 i `) J | 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.& c/ r7 Z0 }( f3 d1 b! g 0 Y" V2 \# ?7 E* B* y8 C) uHuang, R. X., 1990. On the structure of inertial western boundary currents with two moving layers.   Tellus, 42A, 594--604. ) K) J! S2 |# }" A. u6 N5 `! o ' U- }; ^# ~6 W5 a) B% x+ BHuang, R. X. and H. M. Stommel, 1990. Cross-sections of two-layer inertial Gulf Stream.   J. Phys. Oceanogr., 20, 907--911.. r3 i9 v+ U) H 6 R/ g2 ^5 M6 K, [Huang, R. X., 1990. Matching a ventilated thermocline model with inertial western boundary currents.   J. Phys. Oceanogr., 20, 1599--1607. ' v% i$ } ]! o' a9 B3 S9 I; d2 Z# T- {9 _ 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--540.6 v" |/ U5 ^3 l% s , o9 F3 ?- t9 T$ X5 h9 p7 [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. ( ?: T# L' g, \+ n6 R l6 ^; g I: \( X( o( B( _( t+ r7 e3 K# [ 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. * s7 x1 }6 J& @6 q D1 }; D% f * o) O' K' w9 s3 fHuang, 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., u) o1 P* k7 I( g# w 6 i/ E% r# a/ v8 B5 z1 ?2 x 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. * w8 g4 a6 K( H% c$ a: j1 @# ^2 n* [- [9 I3 k Huang, R. X., 1993. A two-layer model for the wind and buoyancy forced circulation. J. Phys. Oceanogr., 23, 104--115. / H3 R! d4 f& e 0 `% E+ J! A" c7 s9 M( |4 u( \. LHuang, R. X. and R. W. Schmitt, 1993. The Goldsbrough—Stommel circulation of the world oceans.   J. Phys. Oceanogr., 23, 1277--1284.7 d# b/ h) g4 V( k- x, f 1 ~( E) t. ^# A7 X! T/ v 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. 3 p, u; O0 B' R/ A+ ?9 q" o1 e' V/ r0 j! n 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. ! c7 e, p4 R; R/ b# _" S) {" ` u* ^- E$ S* f; ?+ \$ e Huang, R. X. and R. L. Chou, 1994. Parameter sensitivity study of the saline circulation. Climate Dynamics, 9, 391-409.6 X: k" L- z8 l+ D: q) C2 Z + c+ n, @% h1 w Huang, R. X., 1994. Thermohaline circulation: Energetics and variability in a single-hemisphere basin model. J. Geophs. Res., 99, (C6), 12,471-12,485. P* n; a0 t* @& @! Z% t- K: v3 O& @! C% c. H3 T+ o) X 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. ) g. h6 b# A* ~& {! S$ I3 `! c3 `( U/ U' ?: i Wang, L. P. and R. X. Huang, 1994. A simple model of abyssal circulation in a circumpolar ocean. J. Phys. Oceanogr., 24, 1040-1058. " @* `+ f9 Q1 o) P4 }5 U8 c8 b9 h- V/ D8 H% h7 L. z7 Z Huang, R. X. and S. Russell, 1994. Ventilation of the subtropical North Pacific. J. Phys. Oceanogr., 24, 2589-2605. : i( o% w8 T1 N, w) ^. ?6 y* P5 ?" b. i% [ 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.! I% R; Q# k n" m d- Q. G" p % b4 u4 c5 m# t$ W1 ^5 [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.( Z8 T5 G4 A) o3 z* l7 v h2 {1 N- M* `4 {% g# M( \8 a Pickart, R. and R. X. Huang, 1995. Structure of an inertial deep western boundary current. Journal of Marine Research, 53, 739-770.9 o$ S. C5 X$ `5 e( I8 p; N! P " {6 M! `8 G( r# wQiu, B. and R. X. Huang, 1995. Ventilation of the North Atlantic and North Pacific: Subduction vs. Obduction. J. Phys. Oceanogr., 25, 2374-2390. ; z/ R0 y* Q& [# R, ]& S7 _- x- v# k7 C Huang, R. X. and J. R. Luyten, 1996. Reply. J. Phys. Oceanogr., 26, 286. + m* V" r# ^2 `' \* D# B" p5 j 8 G# n* e; @5 A Dewar, W. K. and R. X. Huang, 1996. On the forced flow of salty water in a loop. Physics of Fluids, 8, 954-970. + p3 b5 t5 ~1 |7 C& k X; D/ q% u( y* `1 u# z7 G 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. 2 S- g7 X- C+ {* a: D% w7 Y# g- v; c q, h; L% [ Huang, R. X. and W. K. Dewar, 1996. Haline circulation in a loop model: bifurcation and chaos.   J. Phys. Oceanogr., 26, 2093-2106./ y; X( G( L8 \. a( d$ S! P1 | % v* R6 ^6 v: o% ?Huang, R. X. and J. Yang, 1996. Deep-water upwelling in the frictional western boundary layer. J. Phys. Oceanogr., 26, 2243-2250. 8 u6 y! a, @' K7 ` O 4 `( H4 Q& l9 P! w, ?. V6 [% `Huang, R. X., 1998. Available potential energy in a Boussinesq ocean, J. Phys. Oceanogr., 28, 669-678. ' K( Q `5 B5 F6 J ( w/ T7 f2 d0 t' b! _( QHuang, R. X., 1998. On the energy balance of the oceanic general circulation.   Chinese Journal of Atmospheric Science, 22, 452-467. 3 ?' Q# s$ ^* S& f) P6 V" ?/ l0 P- h* r' n" o! G; H! Z# g Huang, 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. 6 B+ Z6 c- _2 M% e6 i ( X( A0 q) h) H' j- PWang, L. and R. X. Huang, 1998. A homogeneous model of the Decon cell in a circumpolar ocean. Dyn. Atmos. Oceans, 28, 157-177. / }* T# r! f, N! I" A/ L" S* M# `8 P" F5 u- H) V Zhang, J., R. Schmitt, and R. X. Huang, 1998. Sensitivity of the GFDL Modular 1 J( {' b. Z" [3 A$ Z6 G" b3 w Ocean Model to parameterization of double-diffusive processes, J. Phys. Oceanogr., 28, 589-605. 3 {+ r8 m* e% ^4 t# h8 V $ ?: p) `, c, U" G$ oKelly, 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 Y- f% l% `% x* x2 P& N q# O8 z$ Q7 `' g3 |; \. y2 p8 R Huang, R. X., 1999. Mixing and energetics of the thermohaline circulation.   J. Phys. Oceanogr., 28, 727-746. 7 l! L4 e5 e7 z7 Y0 ^# D, k. [& F3 C6 G# n; S- g 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. . q! J& t4 |3 V% r0 E- t % n, P. d# x1 z4 ~% A. T, HJin, 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.. ^( e5 f- R& |! @ 3 E9 n ~8 m4 m1 n: G7 z# u Huang, R. X. and J. Pedlosky, 1999. Climate variability inferred from a layered model of the ventilated thermocline, J. Phys. Oceanogr., 29, 779-790. 9 ?$ U+ Y. Y! h" e+ n - K' V$ \$ R* E' A' e; aHuang, R. X., 2000. Climate variability inferred from a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 389-1406. % [% u+ o* P0 o( n! d, m4 C$ J2 A Huang, R. X., 2000. Parameter study of a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 1372-1388. ; A: Y1 Z9 v5 z - |2 y3 }, T4 B: C3 x2 n$ ]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.) j$ ]: j" ?7 q1 M# ^ $ Q6 W( m3 \- E6 h3 {2 p 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. ; k6 k: }& A$ @8 ~ ! V. d9 y3 v# I _, ]. y4 hHuang, 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.: f: w# X4 W6 i + V9 J: q5 q% v7 n1 YHuang, 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. / Y0 |) m) P7 [6 A) o# U& H; M 0 Z- z4 V0 c+ ^( D+ GHuang, Rui Xin, 2001. An analytical solution of the ideal-fluid thermocline. J. Phys. Oceanogr., 31(8), Part 2, 2441-2457.8 r# H4 v8 F3 P+ _ 9 [. ^, ^3 z8 A- d& X2 G( j. e4 O4 ODewar, W. K, and R. X. Huang, 2001. Adjustment of the ventilated thermocline. J. Phys. Oceanogr., 31, 1676-1697. 5 ~ q# v1 L2 |; L7 A- y# K. x 1 w; y$ M$ P$ N8 z7 k p7 ~Huang, R. X., and Q. Wang, 2001: Interior communication from the subtropical to the tropical oceans. J. Phys. Oceanogr., 31, 3538-3550./ K) h1 j0 M: j& {, h ' T- w) B3 O) `1 L: N! t 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. 9 w) l+ S9 I% {" c& K' [( X( w( j$ @$ l. K& k% ^; }. T Huang, R. X. and J. Pedlosky, 2002. On aliasing Rossby waves induced by asynchronous time stepping. Ocean Modelling, 5, 65-76./ W6 `( p9 Z, w3 Y0 f# \ , A' O3 _* |8 Z( D( e, ~# [- _Huang, 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. 1 I, u+ X& k0 u/ R 4 k, w. Z6 `# i% _, ^$ d* d 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. 8 J g# |! S+ T& E# i1 v; }3 P: y; {, P Zhang, 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). 4 K. |% `& a2 T6 r1 d# Z4 ~8 n3 g3 B7 O5 v; o+ t, I 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. / P+ G1 Q) z; b9 G; v' @ * ~& a8 `7 t, a, C. N* V6 }Wang, W. and R. X. Huang, 2004. Wind energy input to the Ekman Layer. J. Phys. Oceanogr., 34, 1267-1275. 1 o4 ~5 l/ E; W9 D" B1 v1 i9 q% w* W: \; H8 \+ G0 l Wang, W. and R. X. Huang, 2004. Wind energy input to the surface waves. J. Phys. Oceanogr., 34, 1276-1280. 3 [6 G) v+ L) B5 [% d% }+ `3 ?# ?$ x! s E$ d+ {7 T Huang, R. X., 2004. Ocean, energy flow in. C. J. Cleveland (Ed.) Encyclopedia of Energy, Elsevier, Vol. 4, pp 497-509.( F% r- L- `: P. `1 @+ K ! _1 J3 @7 f& q% H+ l Huang, R. X., 2005: Available Potential Energy in the World Oceans, J. Mar. Res., in press. & w, M4 [: P# d; V- E5 E& h . D' n( ?0 q7 XWang, Q. and Rui Xin Huang, 2005: Decadal Variability of Pycnocline Flows from the Subtropical to the Equatorial Pacific, J. Phys.Ocanogr., in press.$ ~* `7 N3 |: p0 N/ b, P4 A / j2 n8 @; j1 [" p" E$ AWang W. and R. X. Huang, 2005: An experimental study on thermal circulation driven by horizontal differential heating, Journal of Fluid Mechanics, in press. 0 k3 Q, L' J6 C2 M M9 V3 c/ m 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.! u O& r% P3 |) a) r $ k( w4 k1 r7 u 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.9 C/ X- A8 U) |" v& q 8 C4 ? A% e+ @# N6 R 0 [1 ~" \+ f( [5 E5 ^/ b0 a7 tNon-Refereed Publications: Z1 }$ I b2 ^4 g9 c7 ] . f6 I4 E& |+ f; c6 L% HHuang, R. X., 1976. Some problems in the supersonic stream—surface theory.   Information of Mechanics, No. 2 (in Chinese). 3 c+ L Q8 p. n1 T( P8 |# ~1 `4 B0 C4 k+ N Huang, R. X., 1977. On the stream--surface theory. Information of Mechanics, No. 1 (in Chinese). ( N6 Q- r3 L/ }$ g, }% w # ]5 B1 q! s( yHuang, 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). ) ?: t/ u6 X8 o# B# s 9 Q' S0 B4 q, FHuang, R. X., 1980. On the one--dimensional approximation of viscous fluid flow. Progress in Mechanics, No. 3 (in Chinese). ! d! ~' `, u; ?% L+ f# D & N7 K* h1 z1 [4 s JHuang, R. X., 1992. Deep western boundary currents. Oceanus, 35, (2), 26-27." M Q; C" t6 L- { ( N, u) f6 d- Q7 C7 iHuang, R. X., 1992. Freshwater driving forces---A new look at an old theory.   Oceanus, 35, (2), 36-37.0 |5 b/ q+ Q: l0 {- h 2 {" |, u) F7 W4 g$ x: p2 Z' q Huang, R. X., 1992. A trip to the MBL Library with Hank. Oceanus, 35, (Special Issue: A Tribute to Henry Stommel), p. 126.5 c5 d x* f! @% w0 b. s ) ~9 x2 A) ~* }. c; g1 i8 @7 uHogg, N. G. and R. X. Huang (editors), 1996. Collected Works of Henry M. Stommel (3 volumes, 1943 pp), American Meteorological Society.0 m3 t6 S* [7 `% W % A4 B8 y( q8 ]6 s/ UHuang, R. X. and J. Yang, 1996. Oceanic Aspects of the Climate Modeling, Oceanus, 39, (2), 36-38.* n1 y* t+ B" @( L/ L7 @8 ^ 2 t$ J/ i: H3 E# A% Z Huang, R. X., 1998. The future of physical oceanography, a personal view. A speech at the NSF-sponsored Physical Oceanography Workshop. ! W, c% |3 p" u$ c. L- T1 t0 E# [ 3 p5 C2 G/ j7 ]. K+ {' ?6 {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. # J1 r" k7 k9 J/ |1 P' r! \' h* n2 m- R. M W. Wang and R. X. Huang, 2004: Wind energy input to the surface waves and Ekman layer, Bull. Amer. Meteo. Soc., 85, 818-819. & U4 W. H0 `9 k + i$ l* b6 t. [& kTechnical Report0 x0 L h: A7 a# o6 G 5 |% k9 V* o! k4 N, B+ DHuang, 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 ! v6 P# z+ @7 P% NTechnical Report WHOI--83--41, 106./ n$ A+ }5 L, c. K% y7 ^ 7 w4 S5 y5 t) k* M1 h: D6 t- R Contributor to Chapter 5: Climate Models-Evaluation in "Climate Change 1995", The Intergovernmental Panel on Climate Change, World Meteorological Organization / United Nations Environment Program, 1996.# Q" ?! O( H( A/ p) n . {# d E9 K! }' Y- R6 q Book Reviews. i* ~& i( [/ B& W6 y- f$ a0 o ! }0 _$ d+ r M, z 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. 0 |; w* b# o* N4 ?' W, D2 t8 k: q+ ]. [9 q/ O 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), 775.9 S; i0 ?. x8 ~ + o& ]) C; S2 [& P, N Huang, R. X., 1997. Review of Introduction to Physical Oceanography by George Mellor. American Journal of Physics. - C' k# @0 b! _- n; ~9 }7 I2 Y9 H2 {4 m4 ~, l5 K2 N Thesis * ^' y* J/ s$ [) z; D" r5 Q) b' t) r: b0 [+ m9 I 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.) K1 d. i4 H% C: G ; W1 N7 O2 \& J8 ^Lecture Notes2 J7 x0 ^% H* }$ _ & f8 x0 ?+ H7 b! u' M+ THuang, 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. ( i) R4 Y. K3 e" @% B" W 0 d! l* @# L& W7 t% ~( h) s+ X8 k, d5 B" fHuang, 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. ) c, _5 o9 N5 y5 v : Z1 r7 C+ Z- o5 v7 B6 lHuang, 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. & M: `0 Q6 B' H Q- K1 _1 A3 y9 U% tHuang, 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. / O4 ?' ], ]& E& s" I7 s! U; n1 |0 E 9 w" I) {* `7 P( e* dReference Book 0 x2 [* @! W3 U- N# [% F4 j& p8 D& Y1 O- e$ s/ D) c' u' b 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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