b
Volume of the air bubble, $V_{1}=1.0 cm ^{3}=1.0 \times 10^{-6} m ^{3}$
Bubble rises to height, $d=40 m$
Temperature at a depth of $40 m , T_{1}=12^{\circ} C =285 K$
Temperature at the surface of the lake, $T_{2}=35^{\circ} C =308 K$
The pressure on the surface of the lake:
$P_{2}=1 atm =1 \times 1.013 \times 10^{5} Pa$
The pressure at the depth of $40 m$
$P_{1}=1 atm +d\rho g$ Where $, \rho$ is the density of
water $=10^{3} kg / m ^{3} g$ is the acceleration due
to gravity $=9.8 m / s ^{2}$
$\therefore P_{1}=1.013 \times 10^{5}+40 \times 10^{3} \times 9.8=493300 Pa$
We have: $\frac{P_{1} V_{1}}{T_{1}}=\frac{P_{2} V_{2}}{T_{2}}$
Where, $V_{2}$ is the volume of the air bubble when it reaches the surface $V_{2}=\frac{P_{1} V_{1} T_{2}}{T_{1} P_{2}}$
$=\frac{(493300)\left(1.0 \times 10^{-6}\right) 308}{285 \times 1.013 \times 10^{5}}$
$=5.263 \times 10^{-6}\; m ^{3}$ or $5.263 \;cm ^{3}$
Therefore, when the air bubble reaches the surface, its volume becomes $5.263 \;cm ^{3} .$