Table 3 Parameters used to estimate τ y,cr and τy,cr′ for Earth as in Solomatov ( 2004a ,b)
α | 3×10−5 |
κ | 10−6 m2 s −1 |
δ lid | 100 km |
k | 3 W m −1 K −1 |
E | 430 kJ mol −1 |
d | approximately 500 km |
g | 10 m s −2 |
ρ | 3,300 kg m −3 |
T 0 | 300 K |
T i | 1,700 K |
l hor | 100 km |
α | 3×10−5 |
κ | 10−6 m2 s −1 |
δ lid | 100 km |
k | 3 W m −1 K −1 |
E | 430 kJ mol −1 |
d | approximately 500 km |
g | 10 m s −2 |
ρ | 3,300 kg m −3 |
T 0 | 300 K |
T i | 1,700 K |
l hor | 100 km |