Initial tests 12 for the GCR (balanced variable)
This page is repeated in both frames to allow comparison between figures.
Characteristics of this test:
- RHS PV is raw data.
- Grid-only PV (not grid/normal mode hybrid).
- The first guess is streamfunction after vertical regression (Gp).
- Diagonal preconditioning.
- 50 iterations (restart 5).
- Mass weighted inner product for GCR coefficients.
- Data location /export/custard/disk-01/ross/PV_Results/GCR_Test/PV/RevisedTest/GridOnly_MassWt_PreCon
Notes about the plots on this page:
- For each variable, horizontal (long/lat) and vertical (lat/eta) plots are shown.
- For PV variables the extra modes are shown in addition.
- For the horizonal plots, the level is L30 (eta=0.445).
- For the vertical plots, the longitude slice is Greenwich meridian.
- Each field (except for the PV modes) is decomposed into large horiz/small vert (left) and small horiz/large vert (right) scales.
- The plots show the max, min, and mean (calculated by the plotter).
- Plots of balanced pressure have been shown without density scaling in the linear balance equation (to allow us to see the vertical structure). This is for diagnostic purposes only - the actual density scaled pressures are used in the calculations.
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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