Number of profiles | Number of data | AVE | RMSD | MAXD | MIND |
---|---|---|---|---|---|
20 | 6025 | 0.35 | 0.97 | 8.56 | -3.57 |
Abbreviations in the table indicate:
AVE: average difference (observation value minus assimilation value)
RMSD: root mean square of difference
MAXD: maximum difference
MIND: minimum difference
Depth range | Number of data | AVE | RMSD | MAXD | MIND |
---|---|---|---|---|---|
0-50 | 500 | -0.12 | 0.39 | 1.80 | -1.10 |
50-100 | 488 | 0.44 | 1.64 | 8.10 | -2.43 |
100-150 | 475 | 0.81 | 2.05 | 8.56 | -3.57 |
150-200 | 475 | 0.59 | 1.49 | 6.33 | -1.90 |
200-250 | 475 | 0.31 | 0.95 | 2.91 | -1.96 |
250-300 | 475 | 0.36 | 0.65 | 2.17 | -1.33 |
300-350 | 475 | 0.35 | 0.46 | 1.17 | -0.85 |
350-400 | 475 | 0.31 | 0.40 | 1.08 | -0.74 |
400-450 | 475 | 0.34 | 0.26 | 0.88 | -0.18 |
450-500 | 475 | 0.34 | 0.26 | 0.91 | -0.04 |
500-550 | 186 | 0.34 | 0.33 | 1.02 | -0.11 |
550-600 | 175 | 0.33 | 0.34 | 1.17 | -0.30 |
600-650 | 162 | 0.31 | 0.30 | 1.21 | -0.28 |
650-700 | 158 | 0.26 | 0.26 | 0.96 | -0.19 |
700-750 | 150 | 0.24 | 0.20 | 0.70 | -0.06 |
750-800 | 150 | 0.26 | 0.24 | 0.82 | -0.15 |
800-850 | 141 | 0.23 | 0.23 | 0.77 | -0.15 |
850-900 | 111 | 0.22 | 0.20 | 0.63 | -0.18 |
900-950 | 4 | 0.22 | 0.25 | 0.54 | -0.17 |
950-1000 | 0 | - | - | - | - |
Error data: 0 of 669
On land: 0 of 20
Invalid position: 0 of 20
Error data (low): 0 of 669
Error data (high): 0 of 669
Error data: 0 of 669
◊Station map | ◊Vertical temperature profile Vertical profile of temperature along the observing line of PX11 moved the entire profile by 5 degree Celsius. |
◊Vertical observation sections | ◊Summary of differences (Obs. - Assim.) by depth Dots and error bars represent the averages and root mean squares of the differences, respectively. Crosses represent the maximum/minimum differences. |
◊Vertical sections for the result of assimilation by MOVE-NP | ◊Distribution of differences (Obs. - Assim.) by depth |
◊Vertical sections of differences (Obs. - Assim.) | ◊Distribution of differences (Obs. - Assim.) by temperature |