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15 Jan 2020: Table: Errors for n = 20 Figure: Errors for n = 15The growth in the error is explained by the product term in (1.1) (the rightmost column of the table).

7 Oct 2020: Ah‖ 1 as h 0 the method is stable. 20 / 21.

4 Feb 2020: The initial condition. M = δ(r r0) g =Ar. 1/20. 2πδ(y y0).

24 Sep 2020: When concentrated φ > 20%, they also impact layer above andbelow, leading to a similar pressure σyy σxx (force-chains at 45to flow), so N1 0.

29 Oct 2020: t= Lu(x,t), x [1, 1], t 0 ,. u(x, 0) = g(x), x [1, 1],(3.20). ... for any time step τ > 0.For general linear operator L in (3.20) with constant coefficients, the matix B is again diagonal.

26 Oct 2020: 20. Method 2.36 (Splitting of inhomogeneous systems) Recall our goal, namely fast methods for the two-dimensionaldiffusion equation. ... where b originates in boundary conditions (and in a forcing term f(x,y) in the original PDE (2.20)).

1 Mar 2020: 2) Γs(N N), (20). where N represent the densities of the incoherent reservoirs of spin-up and spin-down excitons providing gainto the condensate through stimulated bosonic scattering, γC characterizes

10 Mar 2020: A =. 2 4 70 3 10 0 20 0 10 0 2.

6 Jul 2020: 20, consistent withstudies in macroscopic flows [7,9,10] that used the appa-ratus scale (millimeter) for reference. ... I. Labo-ratory studies, IEEE J. Oceanic Eng. 20, 147 (1995). [10] M.

4 Feb 2020: 9.35. o. 0.10. I. I. I. I. el 5 10 15 20. ... 0.28. 0A$ -. 0.10 -. 0.05. 0.00. -e.05. -•.15. -•.20. x.