Initial tests 22 for the GCR (unbalanced variable)
This page is repeated in both frames to allow comparison between figures.
Characteristics of this test:
- RHS anti-PV is raw data (does not include extra f factor).
- PV=0 transform is grid only.
- The first guess unbalanced pressure is zero.
- Diagonal preconditioning.
- 500 iterations (restart 5).
- Mass weighted inner product for GCR coefficients.
- Data location /export/custard/disk-01/ross/PV_Results/GCR_Test/antiPV/GridOnly_PreCon_500_no_f_Zero_Guess1/
Notes about the plots on this page:
- For each variable, horizontal (long/lat) and vertical (lat/eta) plots are shown.
- For the horizonal plots, the levels are "bottom level" = L1 (eta=0.00025), "lower level" = L11 (eta=0.056) and "upper level" = L30 (eta=0.445). There are 38 levels in total.
- For the vertical plots, the longitude slice is Greenwich meridian.
- Each field (except differences) 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).
- Unbalanced pressure is also plotted as the difference between the 'solution' and the initial guess.
- Anti-PV is also plotted as differences: 'solution'-'RHS', 'initial'-'RHS' and 'solution'-'initial'.
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
1. Initial guess unbalanced pressure perturbation (ref: Ap_1)
Horizontal plots at L30
Horizontal plots at L11
Horizontal plots at L1
Vertical plots at Greenwich meridian
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
2. Intial Anti-PV (ref: antiPV_Initial)
Horizontal plots at L30
Horizontal plots at L11
Horizontal plots at L1
Vertical plots at Greenwich meridian
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
3. RHS Anti-PV (ref: antiPV_RHS)
Horizontal plots at L30
Horizontal plots at L11
Horizontal plots at L1
Vertical plots at Greenwich meridian
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
4. The solution in terms of unbalanced pressure (ref: Ap_Solution)
Horizontal plots at L30
Horizontal plots at L11
Horizontal plots at L1
Vertical plots at Greenwich meridian
Difference plots for vertical plot, L11 and L30
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
5. The solution in terms of antiPV (ref: AntiPV_Solution)
Horizontal plots at L30
Horizontal plots at L11
Horizontal plots at L1
Vertical plots at Greenwich meridian
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
6. Difference of anti-PV: Solution - RHS
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
7. Difference of anti-PV: Initial - RHS
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
8. Difference of anti-PV: Solution - Initial
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
9. Unbalanced streamfunction of the solution (zero PV)
Horizontal plots at L30
Horizontal plots at L11
Horizontal plots at L1
Vertical plots at Greenwich meridian
Jump to:
1(Ap_1)
2(antiPV_Initial)
3(antiPV_RHS)
4(Ap_Solution)
5(AntiPV_Solution)
6(Solution-RHS)
7(Initial-RHS)
8(Initial-Solution)
9(Unbal_Psi)
Convergence
The convergence (Error norm vs total iteration)
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