Initial tests 17 for the GCR (balanced variable)


This page is repeated in both frames to allow comparison between figures.



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

Characteristics of this test:

Notes about the plots on this page:


Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

1. The raw pressure perturbation (ref: p)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

2. The raw theta perturbation - hydrostatic balance with 1 (ref: Theta_p)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

3. The raw vorticity perturbation (ref: Vort)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

4. The raw streamfunction perturbation (ref: psi)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

5. The pressure in balance with 4. (ref: Gp)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

6. The theta in hydrostatic balance with 5. (ref: Theta_Gp)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

7. The PV calculated from 4. and 5. (ref: PV)

Horizontal plots at L30

Vertical plots at Greenwich meridian

PV modes



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

8. The filtered streamfunction perturbation (ref: psi_filt)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

9. The pressure in balance with 8. (ref: filtered_Gp)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

10. The theta in hydrostatic balance with 9. (ref: filtered_Theta)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

11. The PV calculated from 8. and 9. (ref: filtered_PV)

Horizontal plots at L30

Vertical plots at Greenwich meridian

PV modes



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

12. The PV calculated from raw data (ref: PV_RHS)

Horizontal plots at L30

Vertical plots at Greenwich meridian

PV modes



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

13. The 'solution' streamfunction perturbation (ref: Solution)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

14. The pressure in balance with 13. (ref: final_Gp)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

15. The potential temperature in balance with 14. (ref: final_Theta)

Horizontal plots at L30

Vertical plots at Greenwich meridian



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

16. The PV calculated from 13. and 14. (ref: final_PV)

Horizontal plots at L30

Vertical plots at Greenwich meridian

PV modes



Jump to: 1(p) 2(theta_p) 3(Vort) 4(psi) 5(Gp) 6(theta_Gp) 7(PV) 8(psi_filt) 9(filtered_Gp) 10(filtered_theta) 11(filtered_PV) 12(PV_RHS) 13(Solution) 14(final_Gp) 15(final_theta) 16(final_PV) Convergence

The convergence (Error norm vs total iteration)


Please note that the first 500 iterations only are shown as there is no further visible reduction in the error norm for the rest of the 25000 iterations.









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