The effect of finite-amplitude baroclinic waves on passive, low-level, atmospheric constituents, with applications to comma cloud evolutionSALTZMAN, B; CHUNG-MUH TANG.Tellus. Series A, Dynamic meteorology and oceanography. 1985, Vol 37, Num 1, pp 41-55, issn 0280-6495Article

THE INFLUENCE OF DEEP LAYER AND CROSS-STREAM BOTTOM TOPOGRAPHY ON THE INSTABILITY OF A BAROCLINIC OCEAN CURRENTCHUNG MUH TANG.1979; METEOROL. RDSCH.; DEU; DA. 1979; VOL. 32; NO 6; PP. 161-168; BIBL. 12 REF.Article

THE INFLUENCE OF THE TIME CHANGE OF STATIC STABILITY AND WIND SHEAR ON BAROCLINIC WAVESCHUNG MUH TANG.1980; PURE APPL. GEOPHYS.; CHE; DA. 1980; VOL. 118; NO 3; PP. 706-719; BIBL. 10 REF.Article

BAROCLINIC INSTABILITY OF STRATIFIED SHEAR FLOWS IN THE OCEAN AND ATMOSPHERE.CHUNG MUH TANG.1975; J. GEOPHYS. RES.; U.S.A.; DA. 1975; VOL. 80; NO 9; PP. 1168-1175; BIBL. 19 REF.Article

ON THE MERIDIONAL FORM OF BAROCLINIC WAVES IN A TWO LAYER QUASI-GEOSTROPHIC MODELCHUNG MUH TANG.1972; PURE APPL. GEOPHYS.,; SWITZ.; DA. 1972; VOL. 99; NO 7; PP. 150-155; BIBL. 1REF.Serial Issue

BAROCLINIC INSTABILITY OF A CONTINUOUS MODEL AND MULTIPLE-LEVEL MODELSCHUNG MUH TANG.1978; J. METEOROL. SOC. JAP.; JPN; DA. 1978; VOL. 56; NO 4; PP. 309-311; BIBL. 6 REF.Article

THE ROLE OF LATENT HEAT RELEASE IN BAROCLINIC WAVES-WITHOUT BETA -EFFECTCHUNG MUH TANG; FICHTL GH.1983; JOURNAL OF THE ATMOSPHERIC SCIENCES; ISSN 0022-4928; USA; DA. 1983; VOL. 40; NO 1; PP. 53-72; BIBL. 24 REF.Article

Non-quasi-geostrophic effects in baroclinic waves with latent heat releaseCHUNG-MUH TANG; FICHTL, G. H.Journal of the atmospheric sciences. 1984, Vol 41, Num 9, pp 1498-1512, issn 0022-4928Article