In Griffiths electrodynamics, The maxwell stress tensor is used to determine the net force on the northern hemisphere of a uniformly charged solid sphere of radius R and charge Q. To do this, we solve the integral
$$\vec{F}=\int_S\vec{T}\cdot d\vec{a}$$ where S is the closed surface enclosing the entire northern hemisphere and $\vec{T}$ is the Maxwell stress tensor. The result we get is that $$\vec{F}=\int_S\vec{T}\cdot d\vec{a}=\frac{1}{4\pi \epsilon_o}\frac{3Q^2}{16R^2}\hat{z} \, .$$ This is clearly a non-zero net force in the $\hat{z}$ direction. Later in the text though, Griffiths goes on to say that $\int_S\vec{T}\cdot d\vec{a}$ represents the "momentum per unit time flowing in through the surface". But if we have already calculated that $$\vec{F}=\int_S\vec{T}\cdot d\vec{a}=\frac{1}{4\pi \epsilon_o}\frac{3Q^2}{16R^2}\hat{z}$$ in the case of the hemisphere, then that means that a non-zero amount of momentum is flowing in through the surface of the hemisphere at any giving time. But how can this be if we can easily make the assumption that the uniformly charged sphere is static. That is, if we assume that there is some force that is holding the charges together, counteracting their mutual repulsion then the charged sphere remains intact and does not change in time and so its total momentum remains constant. If this is the case, then how can momentum be flowing into the surface enclosing the northern hemisphere? It seems to me like the interpretation of $\vec{F}=\int_S\vec{T}\cdot d\vec{a}$ as the momentum per unit time flowing in through the surface is rendered untenable by this very example? Am I missing something in my interpretation or is griffiths interpretation actually incorrect here?