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Table 1 Summary of nominal models

From: Effects of variation in coagulation and photochemistry parameters on the particle size distributions in the Venus clouds

Altitude (km)

Condition

Value

40

Acid vapor

10 ppmv

40

Water vapor

30 ppmv

40

CCN (involatile)

(Lognormal) N tot = 200 cm3, \(r_m=0.125\,\upmu \hbox {m},\, \ln {\sigma }=2.16\)

40

Droplets

0

60

Acid vapor

Constant supersaturation across boundary

60

Water vapor

1 ppmv

60

CCN

0

60

Droplets

(Lognormal) \(N_{\mathrm{tot}}=600\,\hbox {cm}^{-3}\)

\(0.175\,\upmu \hbox {m}\), \(\ln {\sigma }=2.16\), (Normal) \(N_{\mathrm{tot}}\)=80 cm\(^{-3}\) \(1.14\,\upmu \hbox {m}\), \(\sigma =1.4\,\upmu \hbox {m}\)

80

Acid vapor

Constant supersaturation

80

Water vapor

Constant mixing ratio

80

Particles

0

All

T, P, \(\rho\)

VIRA at five latitudes

40–48

\(K_{\mathrm{diff}}\)

10 m\(^2\)/s

48–54

\(K_{\mathrm{diff}}\)

Gaussian [see James et al. (1997)]

54–57

\(K_{\mathrm{diff}}\)

Gaussian [see James et al. (1997)]

57–80

\(K_{\mathrm{diff}}\)

2 m\(^2\)/s