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CANARINA:
DISPER:
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Algorithmen II · DISPER software Flüsse von Impuls und Nachhaltigkeit:(Briggs, 1975, p. 63): Fb=gvsds2(DT/4Ts) (7) DT = Ts - Ta, Ts Fm=gvs2ds2(Ta/4Ts) (8) Fb<55, (DT)c=0.0297 Ts(vs/ds2)1/3 (9) Fb > 55, (DT)c=0.00575 Ts(vs2/ds)1/3 (10) Fb < 55: xf=49Fb5/8 (11) Fb > 55: xf=119Fb2/5 (12) l(Briggs, 1971, p. 1031), Fb < 55: he=hs+(21.425 Fb3/4/us) (13) Fb > 55: he=hs+(38.71 Fb3/5/us) (14) (Briggs, 1969, p. 59): he=hs+3ds(vs/us) (15) (Briggs, 1971, p. 1031): s=g[(dT/dz)/Ta] (16) Briggs (1975, p. 96): (DT)c=0.019582 Ts vs s1/2 (17) Briggs, (1975), p. 96: xf=2.0715 us s-1/2 (18) (Briggs, 1975, p. 96): he=hs+2.6 [Fb/(uss)]1/3 (19) Briggs, (1969), p. 59: he=hs+1.5[Fm/(uss1/2)]1/3 (20) Briggs (1972), p. 1030: he=hs+1.60 [(Fb x2)1/3/us] (21) (Bowers, et al, 1979) a) instabile: he=hs+[3Fmx/(betj2us2)]1/3 (22) xmax=4ds(vs+3us)/(vsus) para Fb=0 (23) xmax=49 Fb5/8 para 0 < Fb < 55 m2s3 (24) xmax=119 Fb2/5 para Fb > 55 m2s3 (25) b) stabile: he=hs+(3Fm)1/3{sin[x s1/2/us]}1/3[betj2uss1/2]-1/3 (26) xmax=0.5 pi us/s1/2 (27) betj=(1/3)+(us/vs) (28)
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