Initial tests 13 for the GCR (balanced variable)


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











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