From the ideal gas law, which says PV=nRT, you can see that PV is constant if T is constant. So P1*V1=P2*V2, and you already know how to calculate the pressures. Just don't forget to add in the contribution from atmospheric pressure.
If T were constant, that would be all you need to do. However, a more realistic model is to assume an adiabatic process, since there's no heat exchange if the diver rises quickly. If you haven't learned about adiabatic processes yet, don't worry about it. If you have, do you know the equation relating pressure and volume?