It is very important to mention in your case(given in figure), It not only increasing, but growing like a $parabolic$ profile(dotted line).
Adding to paul,
Imagine boundary layer growth as a momentum diffusion process. (air loosing momentum but not the mass in the boundary layers.) momentum diffusion is attributed to the viscosity of the fluid.
To understand this process, let us take the momentum balance for your problem,
It looks like 1D, So,
$ u \frac{\partial u}{\partial x} = - \frac{1}{\rho} \frac{\partial p}{\partial x} + \nu\frac{\partial^2 u}{\partial^2 x}$
we can assume $\nu\frac{\partial^2 u}{\partial^2 y}$ is smaller (imagine you are rubbing your hands one against another, one of them is retarted against another in the rubbing direction.)
also your geometry dont have any curvature. So $- \frac{1}{\rho} \frac{\partial p}{\partial x} = 0$.
now your momentum balance eqn will become,
$ u \frac{\partial u}{\partial x} = \nu\frac{\partial^2 u}{\partial^2 x}$ it is the balance beween convection of your mass by $u$ and diffusion. !!!
It is mathematically interesting equation and restrict yourself for the region $\delta$- boundary layer thickness.
you get good agreement between experiment and this theory, when you assume $\delta = \sqrt{\frac{\nu x}{ U }}$. (this is called similarity solution in boundary layer theory, credited to prandtl).
So your profile grows as $\delta \sim x^{\frac{1}{2}}$.
Coming to second question, now you have curvature on the blades. So, $- \frac{1}{\rho} \frac{\partial p}{\partial x} \neq 0$.
If you know the velocity profile as a function of $x$ around your turbine blade(one can get through potential flow), then, using bernoulli's equation, convert pressure term interms of velocity and function of $x$. (bernoulli's equation appalicable above the edge of the boudray layer $\sim$ inviscid region)
Once velocity polynomial relation is substituted in the momentum balance equation for pressure, work out the similarity analysis (though complicated)to get your boundary layer profile.
To my knowledge,
Tha boundary layer profile over the $isolated$ turbine blade grows very slowely upto 1/4 th of the chord (favourable pressure), and grows faster after(adverse pressure) that if the boundary layer is atatched till the trailing edge.
(adverse pressure region is pron to separation, where boundary layer theory breaks).
In a cascade turbine you have to find the effect of adjacent blades. still you can proceed with the potential flow theory to get velocity in terms of x co-ordinates.