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师资介绍 黄瑞新教授

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黄瑞新教授 % @- f' Q d1 N( r& K 9 h/ P8 i" w8 Y2 m# Q; J 4 e, z/ v2 h4 ]Rui Xin Huang ! g" G9 |& S, N 6 r, d: E# c( h& G& Z/ iSenior Scientist " y7 U9 \+ _+ c- R4 Q) FW. Van Alan Clark, Jr., Chair for Excellence in Oceanography, 2002-; 6 v% l" w0 V- m- X3 |Woods Hole Oceanographic Institution* O% i$ M! ?6 L7 ]1 O0 E ) ~- y. \+ |7 a( n; I, UPhone: (o) 508-289-2532; ( S P3 y, m/ ^3 } FAX: 508-457-2181; ( i# v7 t' p9 j! \* p e-mail address: rhuang@whoi.edu+ I, T* a* m | Date of Birth: Sep. 15, 1942 t. Z& `& M3 j4 @" L5 YCitizenship: U.S.A. Y3 P, D% Y: W) q* n* U* B, _$ d* ~8 P. }! t Education! F4 l- x. H z+ U$ P: \. a+ h, { 5 K" V4 u1 I$ H: `' l0 ~ The University of Science and Technology of China, 1960-65; B.S. in5 o- W; ~, z# M/ ?' x$ A Thermo-physical Fluid Dynamics of Jet Propulsion, 1965. ; i; F3 Y6 `2 J; t, z8 h- p# B; |( w# E6 |" W" }$ A Graduate School, University of Science and Technology of China, Meteorology, 1978-80.( g* o! A" h, j% t 8 U" D( P( a9 y; S! ^ The Johns Hopkins University, Geophysical Fluid Dynamics, Sep. 1980-Feb. 1981. 7 I2 x, l- Q+ }. T. J+ l7 p" o6 e3 o7 `! Y: Z1 v Massachusetts Institute of Technology/Woods Hole Oceanographic Institution, 1981-1984; Ph.D. in Physical Oceanography 1984. - p# ~' k6 e6 p, L % y# k% l, ?4 Y4 d4 e. xExperience1 b2 U6 u% h! j. e5 x. o0 P" P / \. U& M( J3 Z4 B. xResearch Associate, Institution of Mechanics, Beijing, China, / F0 M+ g! X8 @" ` t: [% R T4 M6 |3 w# U+ j# [& v6 X. L M2 W 1965--1978. Self-study of English and mathematics during the 3 H! b O; j1 z" n7 Z5 s8 i$ n Cultural Revolution in China; aerodynamics of wings; transonic flow in # y# A) g: F7 \. d8 i 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. 0 [7 h1 z5 E% X3 [$ E6 W' \6 {* R& E) o8 B$ C7 W8 ]) O+ q8 g( x! p/ r Postdoctoral, M.I.T., 1984. 7 k! A; {) m" L8 w( k- _ Visiting Scientist, Geophysical Fluid Dynamics Laboratory (NOAA), Princeton University, 1984--1986, March--June 1992. . p# j' S* P& [2 l- t- c+ Z9 e, [ s Assistant Scientist, 1986--1990; Associate Scientist, 1990-1998; tenure awarded, 1993, Senior Scientist, 1998-, Woods Hole Oceanographic Institution; g' m6 M, k, S8 g( N 1 d3 ?- s) Y, E5 S% A& N Visiting Associate Professor, University of Hawaii, Jan.-June, 1994.& y6 l1 c- r4 { $ o9 @2 j: ^! {- ?; g8 _: v5 Q5 M' u Visiting Scientist, Cooperative Institute for Marine and Atmospheric Studies,! l& W( h2 Q) M University of Miami, Feb., 1999." r8 L; q3 V, F" G& ^$ F* b1 O : R/ u9 T; R; `( g) H' X% \ Visiting Professor, Lamont-Doherty Earth Observatory, Columbia University, March-May., 1999. $ W2 a2 r- t( W/ T" L * |2 @- J e9 mCorresponding Member, U.S. WOCE Working Group on Numerical Modeling, 1989-1992., R" |- l7 i. F; @7 E0 [ { 6 i$ ]$ s' @$ { Joint Committee of Physical Oceanography, MIT/WHOI Joint Program, 1990-93. ' `- `5 _$ H: e7 j4 U# {' P* C/ h Member, Working Group on Oceanic Thermohaline Circulation and Variability, 3 l3 r9 a/ R. r" m& D. z$ a K0 PClimate System Modeling Project, USA, 1993-96. ( I: F7 h- s3 _" l/ D8 ^" O& K' d# j4 b9 X, y0 ` Member, Climate Change Committee, WHOI, 1995-1999. ' I( n' k) F3 d. V9 q* Z2 O9 U1 R Member, Advisory Committee, Ocean and Climate Change Institute, 2001-2005.7 }6 t) S" d& ?% ~% I) D+ P ( s& j8 X. D4 m0 g- z" {+ y Guest Professor, Ocean University of Qingdao, China, 1996--. ( k4 l$ X& }8 Z. F- l) t ; ?( }$ R ], n# ^Chairman, Academic Committee for the national Key Laboratory of Physical Oceanography, Ocean University of China, 1999-2005. 9 Q% q) @& [ a$ E* v . m7 m" k4 R& c' pMember, 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.+ Y6 z% n9 ~+ h; o 9 ^( o6 \" \0 B; T3 i, cGuest professor, South China Institute of Oceanology, Chinese Academy of Sciences, 2002-.. n7 n6 q+ m/ ]6 F2 O+ `0 a ! B$ u2 O6 n/ c% p 0 K) U9 B4 {1 b: s3 Q5 U4 PTeaching( F( u, u7 Y' n4 P# _6 J ; i' o: D0 z+ M& f0 i! @4 Q( y Steady Circulation in the Oceans and Atmosphere, MIT/WHOI Joint Program, 1988-1991. ) L( C& `- e w% e8 c& y. D! |& w; z, Q1 X3 e Recent Advances in Large-Scale Ocean Circulation Theory, Second Institute of Oceanography, Hangzhou, China, October 7-17, 1992. : E3 d" G1 x9 [6 t9 [ 7 b& E' U% M9 J# ]1 Q$ c( kTheories of the Oceanic General Circulation, University of Hawaii, Spring, 1994. + w m: e3 g' Q. E0 g 0 w, B1 t7 l% X4 g9 J) VAdvances in Theories of Wind-Driven and Thermohaline Circulation, International; z# s. O6 p# c* V 4 b+ A& ~: P3 H: _$ T0 ZSummer School on Ocean-Atmosphere Interaction, July 25-August 4, 1994, Qingdao, China.( v' T& `% A# B7 G 0 ^, x0 z5 B3 [0 f" cTheories of the Oceanic General Circulation, MIT/WHOI Joint Program, * ]8 O; c: R' l* [' t( y2 O$ U7 L& r0 e' B0 T l- t; Z% B/ t Spring 1995, Fall, 1998, Fall, 2001, Spring, 2004. 5 A3 R6 [0 e1 o- v* Z; x' w9 |3 k& m. y' t4 j* K! H t7 c! Y Supervision/ g- K& i7 P" Z' m* G3 T, r 4 A$ a( w, q! Q- I- n/ ?% L$ b4 LServed 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 X6 b" G# U" e2 v: z 4 |4 t5 O7 ^0 B6 pMr. James McLaren, 1987-89; Mr. Li Ping Wang, 1989-93 (Ph.D.); : o/ _/ B6 T+ v; v: C$ s2 p , Y. Y: K, h) o9 U- t) r/ s8 l On thesis committee of other six students, chairman of thesis defense committee for Mr. Hui Ming Zhang and Ms. Sarah Gille. 4 x6 O7 n$ Z. c8 G: { & D4 e$ R- }8 X! t' |! A, wMichael Masterson, Summer Student Fellow, 1987; Marcel Lieberman, Summer Student 4 q' n6 g+ z; a8 C5 FFellow, 1989; Sarah Russell, Summer Student Fellow, 1993. - l- k% n5 H6 [0 v 2 G: J2 Q/ \. } X5 }Sea Cruises 8 r- ~- ]8 |. Q' K# p, m) T- ~2 u/ t; Q! A+ s1 r RV OCEANUS, Seasor test cruise, July, 1989.3 U# l- S0 o4 F Oceanus, Immerges Sea Cruise, August, 2003. ) I* @) X4 F! a 9 O2 E/ d9 }2 b7 ?" G) ], GHonor - [) H' ^% ]" p - [1 f% D4 b' p# J- INominee of President Young Investigator Award, 1989.1 J7 |) J3 H; G0 i# t" c f& i. ~: c& p7 } Research Interest: ; }+ g- u8 K6 C8 g & v4 Z- |. ~3 n1 i3 V, V) a6 y' u" lTheoretical 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. " d! [0 k' Z9 D, T ! c8 C$ @, y5 c# `$ U; P& s LAuthor or co-author of 70 refereed scientific publications. 4 J" R3 q0 ]1 n1 `8 O- {. i3 T8 {* I3 S; Y Refereed Publications: O6 v& }, j; v a/ e9 P5 ?; ` 1 z/ N3 w$ Q6 ]' Y& W6 k3 _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).' Y+ k( D' W$ l1 N , i* n& D$ W, e( @8 B, W Chao, J. P. and R. X. Huang, 1980. The cnoidal waves of a rotating barotropic atmosphere.   Scientia Sinica, XXIII , No. 10, 1266--1277. 4 V" d8 h X8 r, z5 e" |1 N# H4 T& _: S: `8 C2 m. W8 D% @1 j" ] Huang, R. X., 1986. Solutions of the ideal fluid thermocline with continuous stratification.   J. Phys. Oceanogr., 16, 39--59. & x$ n4 c7 g, @2 x% B1 b. y3 m5 H! |' ^0 ^. k Bogue, N. M., R. X. Huang, and K. Bryan, 1986. Verification experiments with an isopycnal coordinate ocean model. J. Phys. Oceanogr., 16, 985--990.6 F* y7 t/ @; m7 F8 S! Z) v / [. V& g$ V& O2 A; }Huang, R. X., 1986. Numerical simulation of wind-driven circulation in a subtropical-subpolar basin. J. Phys. Oceanogr., 16, 1636--1650.% O% u4 ~$ H p8 e. B! o' D 4 Y* f D- l) S 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.+ u8 d$ f: H9 p h4 g- k& q9 L. U 6 ]/ e+ I# c7 RHuang, 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. * z8 I6 ?* q. x( _4 U7 F8 g( e6 g6 C3 ?* i# ` 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. & h4 N& C3 B* s! h" S/ d6 v! m8 J4 v) S 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.* Y* l2 q( G: p ) s( g3 a! F- o5 i% C: zHuang, R. X., 1988. On boundary value problems of the ideal-fluid thermocline.   J. Phys. Oceanogr., 18, 619--641. / B6 p( A- T, \; y4 F4 e! x , R! l; m& F1 a( rHuang, R. X., 1988. Ideal-fluid thermocline with weakly convective adjustment in a subpolar basin. J. Phys. Oceanogr., 18, 642--651.8 p# z& h/ P0 P' U" P 4 h6 N& B2 i" w 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. , h: t w& U4 r5 T( T: J. S9 X" ?: y" [9 h+ G: I9 m3 ^& P 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." `6 @0 q! D, L* P/ i( E 9 _! E3 Z8 ]- i. K) b4 O6 N4 rHuang, R. X., 1989. Simulating the main thermocline in the North Atlantic with an ideal-fluid model.   J. Phys. Oceanogr., 19, 543--547. 5 k; F4 ^0 [. R; D {% T' E2 b1 \$ ?' Y# L# a5 T# |# } 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. + @# y! F# U" u4 [9 s% e$ }. D8 V+ \$ s* ? Huang, R. X., 1990. Does atmospheric cooling drive the Gulf Stream recirculation?   J. Phys. Oceanogr., 20, 750--757.* G2 k; _7 f4 a' S! h8 F : y& W" m/ W% d8 | 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. V3 g; U6 K& Z% M7 n6 j$ @$ V' u 4 Y" p9 N- `7 A+ ^( S, L0 h Huang, R. X., 1990. On the structure of inertial western boundary currents with two moving layers.   Tellus, 42A, 594--604.* Z* r1 R: J5 s+ H# N/ d ' U3 C G! l) G9 V: W& VHuang, R. X. and H. M. Stommel, 1990. Cross-sections of two-layer inertial Gulf Stream.   J. Phys. Oceanogr., 20, 907--911. ) L4 N7 Z, @7 L# |, B" J8 g5 x# n) B4 S* |: ?4 g+ u7 Y Huang, R. X., 1990. Matching a ventilated thermocline model with inertial western boundary currents.   J. Phys. Oceanogr., 20, 1599--1607. / N6 a# D1 b% h # ~- H3 p2 {+ d& [- }; s 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--540.4 T: M3 Z. Q" O$ [; k' ? $ ?7 A" d+ v8 a4 {& g" xHuang, 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--609.3 T5 y6 X' I9 {. E + r5 e# K- F+ x* T% h/ a5 I0 g 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. 5 _5 J2 F5 R# `6 t+ b : s1 k t- I! k5 g4 g( ^/ k% QHuang, 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. 9 o/ V; H0 z# {1 D0 f* L6 p) ~1 W! D7 A S& h- L3 b( t 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--10,036.2 g0 n2 v+ s5 C6 J4 g+ | / j* O& x9 G/ \7 T; w% f: Y, N# bHuang, R. X., 1993. A two-layer model for the wind and buoyancy forced circulation. J. Phys. Oceanogr., 23, 104--115. $ u s" U3 J0 w- P# P3 y 4 @! Z' C7 N) ]2 h$ ~% AHuang, R. X. and R. W. Schmitt, 1993. The Goldsbrough—Stommel circulation of the world oceans.   J. Phys. Oceanogr., 23, 1277--1284./ N( K9 ]: O7 L2 X0 y " g( g. c) v6 R, B- C3 ` 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.' P! }. T! N3 c ! g0 H, U0 {. |. z" AHuang, 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.# a2 J" X& H; {; z 7 @, m4 W/ M3 s+ z( D0 r/ rHuang, R. X. and R. L. Chou, 1994. Parameter sensitivity study of the saline circulation. Climate Dynamics, 9, 391-409.1 ~, `% P" U# o! _' t6 _1 t( u 7 N) M9 b& \7 ^# m; {; [7 a Huang, R. X., 1994. Thermohaline circulation: Energetics and variability in a single-hemisphere basin model. J. Geophs. Res., 99, (C6), 12,471-12,485.8 o$ K# w3 W( ^1 P: r$ {+ L' C 0 X" W* b$ T# }3 {5 U& t1 _2 @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. * ?( i6 Z/ p- K, n9 S& \9 j' }4 n8 G) x" { Wang, L. P. and R. X. Huang, 1994. A simple model of abyssal circulation in a circumpolar ocean. J. Phys. Oceanogr., 24, 1040-1058. 0 I- G# ?6 H1 r* [% E* v# f! E4 g6 b5 G- u2 D Huang, R. X. and S. Russell, 1994. Ventilation of the subtropical North Pacific. J. Phys. Oceanogr., 24, 2589-2605.5 C8 N2 A2 o* z ; [, P6 O& p0 E4 ^" w6 N$ H 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. [, ~: F" L @! o1 J, D; g0 Y 7 v) p( u, K6 t% h: PDewar, W. K. and R. X. Huang, 1995. Fluid flow in loops driven by freshwater and heat fluxes.   Journal of Fluid Mechanics, 297, 153-191. 1 \& i, r0 q8 t; f1 e& ]5 [ {3 v& a z" i$ |$ d) A Pickart, R. and R. X. Huang, 1995. Structure of an inertial deep western boundary current. Journal of Marine Research, 53, 739-770. % F" ?, B# s% r# |# l8 X* Q o/ k$ h& o \4 b# yQiu, B. and R. X. Huang, 1995. Ventilation of the North Atlantic and North Pacific: Subduction vs. Obduction. J. Phys. Oceanogr., 25, 2374-2390.1 ?- H- c9 q6 ^7 H# { - }6 s: C& F1 S) m; KHuang, R. X. and J. R. Luyten, 1996. Reply. J. Phys. Oceanogr., 26, 286. ! D {; D) G) ^0 o2 Q3 \, i t( ~3 V: ?2 u4 E! 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. / Q# e! s/ @( s9 y( H* |2 p+ h6 t8 _8 _, l2 ?* H( O. J! z5 z 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. 6 Z) a% }3 \; P I3 y, c9 p0 I% y% q4 C7 |6 p! ? Huang, R. X. and W. K. Dewar, 1996. Haline circulation in a loop model: bifurcation and chaos.   J. Phys. Oceanogr., 26, 2093-2106. 5 D+ `& M! k7 g( n% J6 A, `# @2 I% d& q; c! f! \# b Huang, R. X. and J. Yang, 1996. Deep-water upwelling in the frictional western boundary layer. J. Phys. Oceanogr., 26, 2243-2250.' |7 q! o% h; T + |9 R1 a4 C; P% i0 tHuang, R. X., 1998. Available potential energy in a Boussinesq ocean, J. Phys. Oceanogr., 28, 669-678. ' t* p% m* h3 j+ s0 o2 v" U0 J: F6 Z/ Q Huang, R. X., 1998. On the energy balance of the oceanic general circulation.   Chinese Journal of Atmospheric Science, 22, 452-467. ; o; B, S5 Y7 R r3 ?$ Z7 ?% R- n+ y4 U3 i) \8 K 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. 8 u' ^* G5 G" l6 {, v+ L3 w: O) {! A' ~! J Wang, L. and R. X. Huang, 1998. A homogeneous model of the Decon cell in a circumpolar ocean. Dyn. Atmos. Oceans, 28, 157-177.- b5 Z! R# U" y" p0 a. H& J 9 P2 q( t5 F8 d4 z- z Zhang, J., R. Schmitt, and R. X. Huang, 1998. Sensitivity of the GFDL Modular ( {/ _3 J) x4 O) A/ E7 B8 c Ocean Model to parameterization of double-diffusive processes, J. Phys. Oceanogr., 28, 589-605. 8 f$ N3 z: f5 K0 u1 p& ^ / F* K5 {: g# |2 w3 H. ~- l 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, 313-327.1 T8 P9 @) Y# Z7 A O8 o8 U - N! M6 B% m7 Q" X: d7 RHuang, R. X., 1999. Mixing and energetics of the thermohaline circulation.   J. Phys. Oceanogr., 28, 727-746. 8 a6 }8 g g! z: x* C/ I+ {) i+ h. O8 G' L" A# M3 U) p5 V 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. & d* T3 u6 U( a8 B$ {6 H: N+ i% I2 b% w 7 r7 ?- E+ e; v: q3 m3 E! h5 gJin, 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. ' t% f+ e, }1 K) s6 n 2 n, E8 f5 m6 y0 p& G( e' _Huang, R. X. and J. Pedlosky, 1999. Climate variability inferred from a layered model of the ventilated thermocline, J. Phys. Oceanogr., 29, 779-790.7 M) I- v: g w5 W) w2 g * C( h8 p: H8 O1 ]3 QHuang, R. X., 2000. Climate variability inferred from a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 389-1406. 8 f+ J( q. B5 c6 i' d1 a * `9 d! e, H+ {6 O Huang, R. X., 2000. Parameter study of a continuously stratified model of the ideal-fluid thermocline, J. Phys. Oceanogr., 30, 1372-1388. 2 |* H% V6 ~) F' W* Z0 V3 \" \( r8 H$ d6 @1 z6 P( h: G 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.) w& p: U- U- b+ N$ n( ^. L ! o A$ L. a! c! S 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. " |3 p7 p4 i& D6 C3 b2 w$ |3 E( E( G5 l0 I6 Y( E8 u3 ^ 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.) ], w( g! H% ?; a# X0 _5 v M2 t " ~7 y' R0 b1 oHuang, 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. / |$ T* Z$ G' }" h3 A, g; \: s7 ~/ M( @& w0 e4 }+ @ Huang, Rui Xin, 2001. An analytical solution of the ideal-fluid thermocline. J. Phys. Oceanogr., 31(8), Part 2, 2441-2457., ~5 j/ t [. C) i5 h z 6 p9 ]; i4 A' l* F6 C9 O Dewar, W. K, and R. X. Huang, 2001. Adjustment of the ventilated thermocline. J. Phys. Oceanogr., 31, 1676-1697. 4 E% H+ x. O2 i! Q' a+ W& f- o G9 \' D2 f: ^ Huang, R. X., and Q. Wang, 2001: Interior communication from the subtropical to the tropical oceans. J. Phys. Oceanogr., 31, 3538-3550./ C+ I) H& G8 y4 ^ ' w- K( Y& ^2 k; [5 w6 p# F& _ 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. & V6 E+ J/ g0 j( T: n+ Z, J+ }' C8 @6 X* y# Z) c S$ V Huang, R. X. and J. Pedlosky, 2002. On aliasing Rossby waves induced by asynchronous time stepping. Ocean Modelling, 5, 65-76. 3 D. w1 Z1 C( M, w / h3 V( r2 N* j9 E! B1 vHuang, 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. % ^) v; w$ {$ W ^5 g Z1 I8 x: B # @5 d' e }, |1 W2 SHuang, 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.: [% L9 A x9 [% Y* X 6 M. L3 k8 `; v- P @# [8 RZhang, 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).: o" c8 y v8 i + [$ W4 z) k8 G, m7 F: U4 x; W 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. & e+ l; F$ J* R+ n# q# A # K% p! k w# sWang, W. and R. X. Huang, 2004. Wind energy input to the Ekman Layer. J. Phys. Oceanogr., 34, 1267-1275.5 h+ g7 B7 l+ ~+ ^ / a& E x, _ X# \ wWang, W. and R. X. Huang, 2004. Wind energy input to the surface waves. J. Phys. Oceanogr., 34, 1276-1280.5 @( ~( o0 M3 U G6 z9 h! s ( S u7 p7 i' KHuang, R. X., 2004. Ocean, energy flow in. C. J. Cleveland (Ed.) Encyclopedia of Energy, Elsevier, Vol. 4, pp 497-509.+ l6 a1 q8 u4 j. q# _" s0 y- C ; s. R6 r5 {# M3 g0 x0 xHuang, R. X., 2005: Available Potential Energy in the World Oceans, J. Mar. Res., in press.* H$ c& D: x. l3 ^) E3 c * N: y; D4 e; ZWang, Q. and Rui Xin Huang, 2005: Decadal Variability of Pycnocline Flows from the Subtropical to the Equatorial Pacific, J. Phys.Ocanogr., in press. 9 l& F$ W' U% U6 g ! e7 j* ` S D8 DWang W. and R. X. Huang, 2005: An experimental study on thermal circulation driven by horizontal differential heating, Journal of Fluid Mechanics, in press. 9 ~8 E- N$ o3 {4 f 6 V7 ^: C6 i5 G2 |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 r% x& b7 o* r& U2 b1 G8 R" V " H- W% U7 C0 }8 T3 B6 e; ^5 C/ T: kHuang, R. X., W. Wang, L. L. Liu, decadal variability of wind energy input to the world ocean, manuscript, submitted to Deep Sea Research II.# P( U; M% n" U6 i' N# p/ k ; q- B/ R+ x* t% U: ` 4 d; A, ^$ @, S/ E, q2 W5 sNon-Refereed Publications , B* G3 { s( ?9 H! s3 i! W! D4 ~/ v Huang, R. X., 1976. Some problems in the supersonic stream—surface theory.   Information of Mechanics, No. 2 (in Chinese). 1 d0 R5 |' T5 ^3 C, h; ]- f, l5 I* P5 | Huang, R. X., 1977. On the stream--surface theory. Information of Mechanics, No. 1 (in Chinese).% v2 i/ ^2 l; l, `- o6 Q4 @ 3 x& X3 m5 r, T1 f0 Q7 [8 E 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). " j: _; c# F& w( n$ Q& z+ K' `/ l . t" ^" G+ t6 S! T x5 g* E3 dHuang, R. X., 1980. On the one--dimensional approximation of viscous fluid flow. Progress in Mechanics, No. 3 (in Chinese).5 F, z6 \$ d3 T3 R 5 J/ L3 H8 E$ g. m( z7 Y Huang, R. X., 1992. Deep western boundary currents. Oceanus, 35, (2), 26-27. 6 n, T8 K4 k3 B. R9 f1 x/ C6 I# Q% P( n$ Y7 F5 c Huang, R. X., 1992. Freshwater driving forces---A new look at an old theory.   Oceanus, 35, (2), 36-37.& p: f. W4 R5 q5 G 3 \- m6 K, ]( z! y1 \, b6 }8 { Huang, R. X., 1992. A trip to the MBL Library with Hank. Oceanus, 35, (Special Issue: A Tribute to Henry Stommel), p. 126. & G+ V; F/ c9 u' e2 b& ~- @4 L2 e) ?2 P# a/ O# E Y Hogg, N. G. and R. X. Huang (editors), 1996. Collected Works of Henry M. Stommel (3 volumes, 1943 pp), American Meteorological Society.* w$ E' H! L2 _, Y0 A% k# q- ^ ; ~8 `$ z6 Y$ b2 m/ C" Q, S% K% V- O Huang, R. X. and J. Yang, 1996. Oceanic Aspects of the Climate Modeling, Oceanus, 39, (2), 36-38. / P% \3 N P0 G+ \4 n* N' S5 U( x, Q5 @9 u Huang, R. X., 1998. The future of physical oceanography, a personal view. A speech at the NSF-sponsored Physical Oceanography Workshop. # M- U% |5 n$ l3 [ j# i- D* r) Z$ t- N1 o 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.: v1 K- m& V7 S 7 G6 ~2 v4 G5 kW. Wang and R. X. Huang, 2004: Wind energy input to the surface waves and Ekman layer, Bull. Amer. Meteo. Soc., 85, 818-819. % N+ H1 L0 F* T( f3 g% f( `) }, |4 \8 J- h$ A8 F Technical Report / Q2 j' Q- ~2 t- H* w 0 h) I- o A5 s* x8 G2 R, D8 }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 4 V- m1 ]1 T0 C, S& jTechnical Report WHOI--83--41, 106.9 ^; @7 i/ n3 L: f & W7 `- k, i% F; M. |5 H- _! f 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.( i, k1 H0 e% l( H! [5 t7 u1 ` - L2 C4 U1 D. P! h. A5 X Book Reviews9 @2 _; ~0 a2 J) ]( L5 {7 c% k: M. b' K a0 q0 A. O) EHuang, 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. % C( U3 m. J- ^3 \/ e O ; n2 o* V4 `9 ?! C, \ HHuang, 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. - ^/ y( G. Y3 a4 {, ~* i" y% @4 ~& _6 J$ {/ f& F Huang, R. X., 1997. Review of Introduction to Physical Oceanography by George Mellor. American Journal of Physics. $ A# ~7 ~. Z: U/ F% ]) W/ c) r: X3 I3 D6 x+ f4 O& Q Thesis! G" m; B; p( b! Y3 S$ y . t/ `1 F. f1 J 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. 2 H+ \8 \% O8 K, V- B: E* K0 z! M! ]; T( K' b" A: p Lecture Notes + q/ ~: V! B4 f5 ?; H _4 X/ G / H+ {6 Y( B) GHuang, 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. F+ N$ ]( _& R3 Z& `; A% |6 ?! i/ m* |4 B! `6 p% ?: \0 d+ B _% {4 } 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. q. p+ L, x/ p- r6 F ' S4 D; ?( @6 ]- X6 r, yHuang, 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. ( g, |% k% j$ A. c" F) I# |; R( X 5 Z% ^5 A* W8 _6 a. jHuang, 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. 8 n, l0 }$ ~1 f" y/ {6 Z _5 n0 Z9 m- q( Y4 I" G Reference Book' j$ H4 t+ l+ j* J 9 W" G0 u( Y9 x u7 KWang, 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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