Looking at gravity field solutions, the errors lead to systematic artefacts located in two bands north and south of the geomagnetic equator.
In Figure 2 we display the numerical solution, the error estimate and the residual for.
Figure 21 Problem (3. 18): The numerical solution, the error estimate, and the residual for.
Figure 6 Problem (3. 8): The numerical solution, the error estimate, and the residual for, and.
The associated root is. Figure 10 Problem (3. 8): The numerical solution, the error estimate, and the residual for, and. Figure 11 Problem (3. 8): The numerical solution, the error estimate, and the residual for, and.
Figure 4 Problem (3. 8): The numerical solution, the error estimate, and the residual for, and. Figure 5 Problem (3. 8): The numerical solution, the error estimate, and the residual for, and.
The associated root is. Figure 7 Problem (3. 9): The numerical solution, the error estimate, and the residual for, and.
The turning point has been found at. Figure 19 Problem (3. 18): The numerical solution, the error estimate, and the residual for.
For this choice of parameters and. Figure 3 Problem (1. 9a - 1.9b): The numerical solution, the error estimate, and the residual for, and.
Finally, based on the integral equation that reflects the relationships between the approximate damped oscillatory solution and its exact solution, the error estimate is given for the approximate damped oscillatory solution.
