Abstract
On the largest scales, planetary climates can be described by their Rossby
number (Ro). Ro is in response to $Gr/Re^2$ , where Gr is the
Grashof number and Re is the Reynolds number. We here simplify $Gr/Re^2$ as h,
where $h=H/H_Earth$ with $H=gP/(2V_e)$ for a planet with surface gravity
g, rotation period P and equatorial velocity
Ve. Unlike h, Ro is difficult to obtain
because of a large diversity in observation. We perform on an in-depth
literature search on average (av) and maximum (mx) wind velocity for each
planet in the Solar system by various observational methods and by altitude. We
explore a correlation between Ro and h expressed as a power
law with index $\alpha$ based on wind velocities of planets in the Solar
system. We obtain a correlation between Ro and h with
$\alpha=0.56$ (av) and $\alpha=0.52$ (mx). Earth's $H=H_Earth$ ($h=1$) is
primarily due to lunar tidal interaction, given our relatively distant
habitable zone (HZ) to the Sun. Our positive correlation, therefore, suggests
exoplanet-moon systems as the `go-to-place' in our searches for potentially
advanced life in exosolar system.
Users
Please
log in to take part in the discussion (add own reviews or comments).