Step 1: Work with occupation fractions instead of the partition function.
Let $p_1$ and $p_2$ be the fraction of the $N$ particles sitting in levels $\epsilon_1$ and $\epsilon_2$ at temperature $T$. Detailed balance for a classical gas in contact with a reservoir gives the Boltzmann ratio
\[ \frac{p_2}{p_1} = e^{-\Delta/k_BT} \]
Step 2: Turn the ratio into normalized fractions.
Since $p_1+p_2=1$, substituting $p_2 = p_1 e^{-\Delta/k_BT}$ gives
\[ p_1 = \frac{1}{1+e^{-\Delta/k_BT}}, \qquad p_2 = \frac{e^{-\Delta/k_BT}}{1+e^{-\Delta/k_BT}} \]
Step 3: Build $U(T)$ from the populations.
The internal energy is just the population-weighted average energy times $N$:
\[ U(T) = N(p_1\epsilon_1+p_2\epsilon_2) = N\epsilon_1 + Np_2\Delta = N\epsilon_1+\frac{N\Delta\, e^{-\Delta/k_BT}}{1+e^{-\Delta/k_BT}} \]
which is the same expression as before, written from the populations rather than from $-\partial\ln z/\partial\beta$.
Step 4: Read off the low- and high-temperature behavior.
At low $T$, $e^{-\Delta/k_BT}\to0$, so $p_2\to0$: almost every particle stays in the ground level and $U\to N\epsilon_1$, a flat plateau.
At high $T$, $e^{-\Delta/k_BT}\to1$, so $p_1\to p_2\to\tfrac12$: the levels become equally populated and $U\to N(\epsilon_1+\Delta/2)$, a second flat plateau.
Between these limits $p_2$ climbs smoothly from 0 to $\tfrac12$, so $U(T)$ rises smoothly between the two plateaus, an S-shaped curve, never overshooting the upper plateau and never decreasing.
Step 5: Rule out the wrong shapes.
Curves that keep growing without bound (options B, D) contradict $p_2$ saturating at $\tfrac12$. A curve that decreases with $T$ (option C) contradicts $p_2$ only ever increasing as $T$ rises.
Final Answer:
The population fractions saturate, so $U(T)$ must saturate too, rising from $N\epsilon_1$ to $N(\epsilon_1+\Delta/2)$ in a sigmoid shape, which is graph (A).
\[ \boxed{U(T):\ N\epsilon_1 \to N\left(\epsilon_1+\frac{\Delta}{2}\right),\ \text{option (A)}} \]