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Optimal excitation of baroclinic wavesFARRELL, B. F.Journal of the atmospheric sciences. 1989, Vol 46, Num 9, pp 1193-1206, issn 0022-4928Article

FINITE-AMPLITUDE BAROCLINIC DISTURBANUS IN DOWNSTREAM VARYING CURRENTS.PEDLOSKY J.1976; J. PHYS. OCEANOGR.; U.S.A.; DA. 1976; VOL. 6; NO 3; PP. 335-344; BIBL. 2 REF.Article

Structure of circulating cells of intensive baroclinic vortices in flows with velocity shears and advective admixture transferDORONINA, T. N.Izvestiâ Akademii nauk SSSR. Fizika atmosfery i okeana. 1995, Vol 31, Num 2, pp 223-232, issn 0002-3515Article

Further study on atmospheric lapse rate regimesSHI-KENG YANG; SMITH, G. L.Journal of the atmospheric sciences. 1985, Vol 42, Num 9, pp 961-965, issn 0022-4928Article

The role of baroclinic eddies in mixing tritium into the oceanic gyres. ReplyAUSTIN, J; GREEN, J; YUAN-HUI LI et al.Tellus. Series B, Chemical and physical meteorology. 1985, Vol 37, Num 3, pp 182-185, issn 0280-6509Article

FINITE-AMPLITUDE BAROCLINIC WAVES IN A CONTINUOUS MODEL OF THE ATMOSPHEREPEDLOSKY J.1979; J. ATMOSPH. SCI.; AUS; DA. 1979; VOL. 36; NO 10; PP. 1908-1924; BIBL. 17 REF.Article

PRISE EN CONSIDERATION DE L'OROGRAPHIE DANS LE MODELE BAROCLINE DE PREVISION D'APRES LES EQUATIONS COMPLETES DE L'HYDRODYNAMIQUE, DANS LE SYSTEME DE COORDONNEES SIGMA .KRICHAK SO.1978; TRUDY GIDROMETEOROL. NAUCH.-ISSLEDOVAT. CENTRA S.S.S.R.; SUN; DA. 1978; NO 196; PP. 62-71; BIBL. 5 REF.Article

CHAOTIC AND PERIODIC BEHAVIOR OF FINITE-AMPLITUDE BAROCLINIC WAVESPEDLOSKY J; FRENZEN C.1980; J. ATMOSPH. SCI.; USA; DA. 1980; VOL. 37; NO 6; PP. 1177-1196; BIBL. 9 REF.Article

INSTABILITY OF NON-ZONAL BAROCLINIC FLOWSNIEHAUS MCW.1980; J. ATMOSPH. SCI.; USA; DA. 1980; VOL. 37; NO 7; PP. 1447-1463; BIBL. 25 REF.Article

THE EFFECT OF BATHYMETRY ON THE STEADY BAROCLINIC OCEAN CIRCULATION.RATTRAY M JR; DWORSKI JG.1978; DYNAM. ATMOSPH. OCEANS; NLD; DA. 1978; VOL. 2; NO 4; PP. 321-339; BIBL. 27 REF.Article

EXPERIENCES NUMERIQUES POUR LA PREVISION DES PRECIPITATIONS CONTINUES SUR UNE AIRE LIMITEE, SUIVANT LE MODELE BAROCLINE DE L'ATMOSPHERE ETABLI D'APRES LES EQUATIONS COMPLETES.ARENS V; KRICHAK SO.1978; TRUDY GIDROMETEOROL. NAUCH.-ISSLEDOVAT. CENTRA S.S.S.R.; SUN; DA. 1978; NO 196; PP. 31-37; BIBL. 6 REF.Article

BAROCLINIC GROWTH RATES OF THE RPN SPECTRAL MODEL.DALEY R; WARN H.sdIN: SOC. METEOROL. CAN. CONGR. ANNU. 10; QUEBEC; 1976; S.L.; DA. S.D.; PP. (1P.)Conference Paper

CALCUL DE LA V DU VENT DANS UNE ATMOSPHERE BAROCLINETSVETKOV VI; TSVETKOVA AA.1980; VESCI AKAD. NAVUK BSSR, SER. FIZ.-MAT. NAVUK; ISSN 0002-3574; BYS; DA. 1980; NO 1; PP. 20-23; ABS. ENG; BIBL. 2 REF.Article

THE EFFECTS OF FRICTION AND BETA ON FINITE-AMPLITUDE BAROCLINIC WAVES.ROMEA RD.1977; J. ATMOSPH. SCI.; U.S.A.; DA. 1977; VOL. 34; NO 11; PP. 1689-1695; BIBL. 7 REF.Article

ON SPATIALLY GROWING BAROCLINIC WAVES IN THE OCEAN.HOGG NG.1976; J. FLUID MECH.; G.B.; DA. 1976; VOL. 78; NO 2; PP. 217-235; BIBL. 20 REF.Article

ANALYSE DE LA NON-STATIONNARITE DU GRADIENT DE TEMPERATURE HEMISPHERIQUE DE L'ATMOSPHEREMARCHUK GI; KURBATKIN GP.1981; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ATMOSF. OKEANA; SUN; DA. 1981; VOL. 17; NO 5; PP. 451-463; ABS. ENG; BIBL. 4 REF.Article

THE DOWNSTREAM AND UPSTREAM DEVELOPMENT OF UNSTABLE BAROCLINIC WAVESSIMMONS AJ; HOSKINS BJ.1979; J. ATMOSPH. SCI.; AUS; DA. 1979; VOL. 36; NO 7; PP. 1239-1254; BIBL. 26 REF.Article

MODELE NUMERIQUE D'EULER-LAGRANGE DES COURANTS DANS UN OCEAN NON HOMOGENESEIDOV DG.1976; IZVEST. AKAD. NAUK S.S.S.R., FIZ. ATMOSF. OKEANA; S.S.S.R.; DA. 1976; VOL. 12; NO 10; PP. 1111-1115; BIBL. 5 REF.Article

BAROCLINIC ROSSBY WAVES AS INFERRED FROM TEMPERATURE FLUCTUATIONS IN THE EASTERN PACIFIC.EMERY WJ; MAGAARD L.1976; J. MAR. RES.; U.S.A.; DA. 1976; VOL. 34; NO 3; PP. 365-385; BIBL. 6 REF.Article

THEORIE DE L'OCEAN BAROCLINE INCLUANT L'EQUATEURKOSNYREV VK; KUFTARKOV YU M.1975; MOR. GIDROFIZ. ISSLEDOV., U.S.S.R.; S.S.S.R.; DA. 1975; NO 3; PP. 29-41; ABS. ANGL.; BIBL. 16 REF.Article

UEBER DEN LEISTUNGSSTAND DES BAROKLINEN MODELLS DES DEUTSCHEN WETTERDIENSTES. ERGEBNISSE DER PRUEFUNG NUMERISCHER VORHERSAGEKARTEN 1970-1972. = EFFICACITE DES MODELES BAROCLINES DU SERVICE METEOROLOGIQUE ALLEMAND. RESULTAT DE LA VERIFICATION DES CARTES DE PREVISION NUMERIQUE 1970-1972BUSCHNER W; OECKEL H; SCHWIRNER JU et al.1973; BER. DTSCH. WETTERDIENSTES; DTSCH.; DA. 1973; VOL. 17; NO 132; PP. 1-38; ABS. ANGL.; BIBL. 4 REF.Serial Issue

EXPERIENCES NUMERIQUES SUR LE CALCUL DES COURANTS ET DE DENSITE DANS LA ZONE EQUATORIALE DE L'OCEANKOROTAEV GK; MIKHAJLOVA EH N; SHAPIRO NB et al.1975; MOR. GIDROFIZ. ISSLEDOV., U.S.S.R.; S.S.S.R.; DA. 1975; NO 3; PP. 15-28; ABS. ANGL.; BIBL. 10 REF.Article

ROLE DE LA BAROCLINITE DES COUCHES PROFONDES DANS LA FORMATION DE LA SURFACE DE NIVEAU DE L'OCEANDEMIN YU L; POYARKOV SG.1975; IN: KOMPLEKSN. ISSLED. MIROVOM OKEANE; MOSKVA; VINITI; DA. 1975; PP. 37-39; BIBL. 2 REF.Book Chapter

Stages in the energetics of baroclinic systemsORLANSKI, I; SHELDON, J. P.Tellus. Series A, Dynamic meteorology and oceanography. 1995, Vol 47, Num 5, pp 605-628, issn 0280-6495Conference Paper

A baroclinic scheme of forecasting tropical cyclone tracksSITNIKOV, I. G; ZLENKO, V. A.Meteorologiâ i gidrologiâ. 1991, Num 3, pp 5-12, issn 0130-2906Article

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