For problems with more than one component, e.g. shallow water equations, the update matrix is an actual matrix and not just a scalar. The normalisation procedure in this case needs to compute the n-th root of this matrix. So far this function is only implemented for scalars.
For problems with more than one component, e.g. shallow water equations, the update matrix is an actual matrix and not just a scalar. The normalisation procedure in this case needs to compute the n-th root of this matrix. So far this function is only implemented for scalars.