“…Essentially, this means that the coarsest grids employed in the multigrid hierarchy must resolve the waves of wave number k. This is however not very useful in practical situations, particularly for large-scale calculations, since then the finest grid is precisely chosen to resolve the waves of wave number k, and one could not use any coarsening at all in a multigrid context. Thus, it is still the case that classical multigrid methods do not work when applied to discretizations of the Helmholtz equation, see for example [20,22] and references therein. Textbooks on multigrid often comment on the difficulty of the case of indefinite problems, for example the early multigrid guide by Brandt and Livne from 1984, which has recently been republished in the SIAM Classics in Applied Mathematics series [10, page 72], contains the quote: "If σ is negative, the situation is much worse, whatever the boundary con-1 This paper is exemplary for a modern paper in numerical analysis: there are several physical problems modeled by PDEs, which are then discretized, and solved by iteration (Richardson iteration, which is almost the Chebyshev semi-iterative method in its original form, albeit constructing an approximate Chebyshev polynomial by trial and error, and Richardson extrapolation), with realistic wallclock times (flops Richardson and his boy calculators were able to attain), computing costs (…”