The two lengths are given by:
$$L_{normal}=L$$
$$L_{summer}=L+\alpha \Delta T L$$
With $\alpha$ the thermal expansion coefficient, $12.0 \times 10^{-6} \: m/m \: K$
Thus the two periods become:
$$Period_{normal}=2 \pi \sqrt{\frac{L_{normal}}{g}}=2 \pi \sqrt{\frac{L}{g}}$$
$$Period_{summer}=2 \pi \sqrt{\frac{L_{summer}}{g}}=2 \pi \sqrt{\frac{L+\alpha \Delta T L}{g}}$$
The ratio between the two is then:
$$\frac{Period_{summer}}{Period_{normal}}=\frac{2 \pi \sqrt{\frac{L+\alpha \Delta T L}{g}}}{2 \pi \sqrt{\frac{L}{g}}}=\sqrt{1+\alpha \Delta T}$$
This can written as the following Taylor series:
$$\frac{Period_{summer}}{Period_{normal}}=\sqrt{1+\alpha \Delta T}=1+\frac{\alpha \Delta T}{2}- \frac{\left(\alpha \Delta T\right)^2}{8} + \frac{\left(\alpha \Delta T\right)^3}{16} - \frac{5\left(\alpha \Delta T\right)^4}{128} + \dots$$
With the first order approximation equal to:
$$\frac{Period_{summer}}{Period_{normal}} \approx 1+\frac{\alpha \Delta T}{2}$$
Assuming that the clock is inside, and the normal temperature is 20°, we have $\Delta T=17 K$. The difference for a day then becomes:
$$\Delta t_{day} \approx 24 \cdot 3600 \cdot \frac{\alpha \Delta T}{2} \approx 9\: \mathrm{seconds}$$ .
This seems like a lot to me, but then again, this is with the assumption that the temperature difference is 17° degrees all day long, which it obviously is not.
If we assume that the temperature varies as a the first half of a sine wave between 20° and 37°, thus providing a time difference of 0 when the temperature is 20°, and $\frac{\alpha \Delta T}{2}$ when the temperature is 37°.
The average expansion is decribed by:
$$\frac{\int_0^{\pi} \frac{\alpha \Delta T}{2} \cdot sin( \pi \cdot t)}{\pi}=\frac{\alpha \Delta T}{\pi}$$
Which amounts to $24 \cdot 3600 \cdot \frac{\alpha \Delta T}{\pi} \approx 5 \: \mathrm{seconds}$ per day , which is still quite a lot.