Time Evolution of the Precipitation Distribution in Experiment S1200
The amount of precipitation is small in the case of Experiment
S1200. Although weak, eastward-propagating disturbances exist at
mid-latitudes that are likely generated by baroclinic instabilities,
and there are also vortex disturbances migrating from the equatorial
region to mid- and high latitudes.
Animation 1: Time evolution of the precipitation
distribution (W/m2) in Experiment S1200. The animation
illustrates the time evolution for a 16-day period in conditions
that are considered to be nearly in equilibrium.
