Step 1: Define Rossby number.
Rossby number measures the importance of inertial (centrifugal) force vs. Coriolis force:
\[
Ro = \frac{U}{fL}
\]
where \(U = 100~\mathrm{m/s},\ f = 10^{-4}~\mathrm{s^{-1}},\ L = \text{radius} = 500~\mathrm{m}.
\]
Step 2: Compute Rossby number.
\[
Ro = \frac{100}{(10^{-4})(500)} = \frac{100}{0.05} = 2000.
\]
Step 3: Interpret.
- If \(Ro \ll 1\), Coriolis dominates → geostrophic balance.
- If \(Ro \sim 1\), Coriolis and centrifugal both matter → gradient wind balance.
- If \(Ro \gg 1\), centrifugal dominates → cyclostrophic balance.
Since \(Ro=2000 \gg 1\), the system is in cyclostrophic balance.
Final Answer:
\[
\boxed{\text{It is in cyclostrophic balance.}}
\]