21 3 Vol.21, No JOURNAL OF TROPICAL METEOROLOGY Jun.,2005 : (2005) : I GOALS/LASG :GOALS AGC
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1 3 Vol., No JOURNAL OF TROPICAL METEOROLOGY Jun.,005 : (005) : I GOALS/LASG :GOALSAGCM :P46. 文献标识码 :A [] GOALS/LASG 9 [] [3~4] 4 R4 300 m 00 m 5 [4] 9 : ;: :ZKCX-SW :969-E-mil: zizwng@mil.i.c.cn
2 [5] II R5L9 I R4L Simmons [6] Hosins [78] η- ( η) = h ( η) + h ( η) () 0 b s 0 0 =000 hp h ( η) hb ( η) s η- ς ( A B V cos ϕ = + ) Ω ( Dsin ϕ + ) + ( F ) h + Fv () cos ϕ λ ϕ D B A U = ( cos ϕ ) + Ω( ςsin ϕ ) ( E + φ ) + ( F ) h + Fv (3) cos ϕ λ ϕ φ ln = RT V η η (4) T T R T( ε0 ε) M ω T T ( V T ) TD η = + + ( T + T + ) + Fh + Fv η c + ε M (5) q = ( V )dη (6) t s η η M M M M = ( V M) + MD η + Fh + Fv (7) η ( ς )(D)( T ') ( q = ln s )( M ) V RT V U RT V A= ςu + η + cos ϕ, B = ςv η η ϕ η λ η η = ( V )dη η η t η (8) ω η = ( V )dη V + ηt η (9)
3 40 R T V = TV T = T( + ε0m) T c * = [ + εm] c V cv ε 0 = ε = R c [9] η-- K + / = A + B (0) / + / + / + / s A + / 6 B + A + / / hp / R4L6 A + / B + / B + / hp A + / / hp B + / / hp A + / / hp B + / / hp = + / / () B = B B () + / / ϕ = φ I + RAT (3) * 0 V Ι 0 A j + / ln j < j / j = α j j = 0 j > α / / = + ln + / [5] + / ( ) = ( B + ln C) s q C A+ /B / A /B+ / / = 9 ω K + / ( ) = [ln ( Vj j) α ( V )] + V ( ) / j= + (4) (5) (6) (7) (6)(8) K K ( η ) + / = B + / ( D + B V q) + ( D + B V q) (8) η j j j s j j j j s j j= j= + (8)
4 F ( η ) = [( η ) ( F F ) + ( η ) ( F F )] (9) η η η + / + / K q = ( D j + j BjV s j q) = s j D RT V RT V cosϕ = [ ( ) + cos ϕ ( )] φ () cos ϕ λ λ ϕ ϕ (0) T T R ω = η + ( T + T ) η c () q () = Dd ( ηt ) (3) ( Tr, qr) n n+ n n+ D r T + T n q + q n = ( RA ( T ) + R( h + h ) ( q )) T = GD q = T δ D A r T C B s sr r + / ( h ) = ( + ln ) / α B j+ / Bj / ( h) = ( Tr Trj( )) sr sr j = j+ / j / R 0, j G = ( T + T ) ( ) + {[ B ][( T ) ( T ) ] j j j r r j + / r + r c, j > 0, j < + [ B ][( T ) ( T ) ]}, j / r r j δ (4) (5) r = (6) sr n n+ n n+ D r T + T n q + q n = x ( RA ( T ) + R( h+ h + T00I0)( q )) t n n+ T D + D n = y+ G( D ) (7) n n+ q T D + D n = z+ δ ( D ) x y z n+ n r n n+ n n n+ n D = D + tx+ tl( l+ ) R ( A ( T + T T ) + ( h+ h + T00I0)( q + q q )) n+ n n n+ n T = T + ty+ tg( D + D D ) n+ n T n n+ n q = q + tz + tδ ( D + D D ) (8)
5 4 R = R/ [ I tll ( + ) R ( A G+ ( h + h + T I )δ ] D = [ I+ tll ( + ) R ( A G+ ( h + h + T I )δ ] D + r T n+ r T n tx+ tl( l + ) R [ A ( T + ty T ) ta GD + ( h + h + T I )( q + tz q tδ D )] r n n r n n n T n 00 0 (8) F = αf (30) 9 n+ n F = ( tα ) F (3) α n+ n F = ( + tα ) F (3) [0~] R4L6 CCM hp 4 00 hp NCEP [] CMAP [3] I R4L9 I R4L9 I R4L9 c (9)
6 hp c b d hp m/s. R4L6 ; b. R4L6 NCEP ; c..d. b. c b d K. R4L6 ; b. R4L6 NCEP ; c..d. b.
7 44 R4L9 3 R4L6 3 d b e c f 3 hp. R4L6 ; b. NCEP ; c. R4L6 NCEP ; d..e. b.f. c.
8 d R4L9 NCEP 4 d b e c f 4 mm/d. R4L6 ; b. CMAP; c. R4L6 ; d..e. b.f. c.
9 46 CMAP R4L9 GOALS/LASG 9 6 I R4L9 SPCZ [4] [5] []. -- [J] [] KANG I S, JIN K, WANG B, et l. Intercomrison of the climtologicl vritions of Asin summer monsoon reciittion simulted by 0 GCMs[J]. Cli Dynmics, 00, 9(4): [3]. [J]. 995, 53(): [4]. [J]. 990, 3(3): [5]. [J]. 999, 3(5): [6] SIMMONS A J, BURRIDGE D M. An energy nd ngulr-momentum conserving verticl finite-difference scheme nd hybrid
10 verticl coordintes[j]. Mon We Rev, 98, 09(4): [7] BOURKE W. A multi-level sectrl model IFormultion nd hemisheric integrtions[j]. Mon We Rev,974, 0 (0): [8] HOSKINS B J, SIMMONS A J. A multi-lyer sectrl model nd the semi-imlicit method[j]. Qurt J Roy Met Soc, 975, 0: [9] WU G X, LIU H, ZHAO Y C, et l. A nine-lyer tmosheric generl circultion model nd its erformnce[j]. Advnces Atmos Sci, 996, 3(): -8. [0] PALMER T N, SHUTTS G J, SWINBANK R, et l. Allevition of systemtic westerly bis in generl circultion nd numericl wether rediction models through n orogrhic grvity wve drg rmeteriztion[j]. Qurt J Roy Met Soc, 986, : []. [J]. 000, (): 3-0. [] KALNAY E, COAUTHORS. The NCEP/NCAR 40-yer renlysis roject[j]. Bull Amer Met Soc, 996, 77(3): [3] XIE P, ARKIN P A. Anlyses of globl monthly reciittion using guge observtions, stellite estimtes, nd numericl model redictions[j]. J Cli, 996, 9(4): [4] SLINGO J M. The develoment nd verifiction of cloud rediction scheme for the ECMWF model[j]. Qurt J Roy Met Soc, 987, 3: [5] LOUIS J F. A rmetric model of verticl eddy fluxes in the tmoshere[j]. Boundry Lyer Met, 979, 7: THE DEVELOPMENT OF GOALS/LASG AGCM AND ITS GLOBAL CLIMATOLOGICAL FEATURES IN CLIMATE SIMULATION Ⅱ The Increse of Verticll Resulotion nd Its Influences WANG Zi-zhi,,YU Ru-cong 3,WANG Peng-fei 3,WU Guo-xiong 3 (. Stte Key Lbortory of Numericl Modeling Atmosheric Sciences & Geohysicl Fluid Dynmics, Institute of Atmosheric Physics, CAS, Beijing 0009, Chin;. Gungzhou Institute of Troicl & Mrine Meteorology, CMA, Gungzhou 50080, Chin; 3. Ntionl Climte Center, Beijing 0008,Chin) Abstrct:In this rt the verticl resolution of the tmosheric comonent of the Globl Ocen-Atmoshere-Lnd System Model of LASG (GOALS/LASG) is incresed bsed on the model with incresed horizontl resolution in rt I of this er. In order to reduce the influences of toogrhy on the strtoshere s the resolution incresed, the energy nd ngulr-momentum conserving hybrid verticl coordinte is estblished, which is lso consistent with other climte models. The hybrid verticl coordinte scheme ssocited with the semi-imlicit method is described in this rt, nd some relted hysicl schemes in the model re lso djusted. Though the min hysicl rocesses remin the sme, the rimry simultion results show tht the verticl structure of tmoshere is more resonble comred with R4L9 in Prt I, nd the wind nd temerture re more consistestent with the observtions. The simulted reciittion nd se surfce ressure re lso imroved obviously. Key words: GOALS; AGCM; model resolution; hybrid-coordinte; climte simultion
GOALS [7] T42 T21 [9 10] R15L9 GOALS - k- Mne Monin-Ouhov [3 7] R15L R42L9 AMIP PCMDI m SSiB 13 [3] Wu [11] 1
21 3 Vol.21, No.3 2005 06 JOURNAL OF TROPICAL METEOROLOGY Jun.,2005 :1004-4965(2005)03-0225-13 1. 100029 2. 510080 3. 100081 : GOALS/LASG 15 R15 42 R42 10 El Niño :GOALS :P461.2 文献标识码 :A (R15L9) [1] [2]
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