Storm Results

Short range models still have a wide
spread of solutions through the short
term period. The integration of T into
X has yielded a partial solution with
an 1/n convergence. We can predict, with
a 26.6% certainty, that all unresolved
variables will converge to 0 when
t = 3.141592

Long range models have a much smaller
variance. Given an average rainfall of
r we can reliably predict that g will
increase proportionally to r, but this
change will be delayed by a t of 67.
This is exciting news, as it means
that we have many options available to
us for increasing the groundwater in
the next generation.

We have eliminated the factor of EM
as a variable in our models by assuming
a para-sympathetic waveform in the
weather cycle. This change increases
the efficiency of our processes by 2.4%