Number of profiles | Number of data | AVE | RMSD | MAXD | MIND |
---|---|---|---|---|---|
25 | 4923 | 0.09 | 0.74 | 4.46 | -2.00 |
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 | 425 | 0.04 | 0.56 | 2.40 | -1.95 |
50-100 | 400 | 0.23 | 1.26 | 4.46 | -1.99 |
100-150 | 400 | -0.51 | 0.83 | 2.61 | -2.00 |
150-200 | 400 | -0.33 | 0.61 | 1.33 | -1.36 |
200-250 | 400 | 0.05 | 0.74 | 1.79 | -1.77 |
250-300 | 400 | 0.35 | 0.92 | 2.80 | -1.48 |
300-350 | 400 | 0.45 | 0.86 | 2.80 | -0.87 |
350-400 | 356 | 0.21 | 0.56 | 2.70 | -0.98 |
400-450 | 350 | 0.16 | 0.43 | 1.07 | -0.88 |
450-500 | 350 | 0.13 | 0.34 | 1.02 | -0.51 |
500-550 | 140 | 0.20 | 0.33 | 1.16 | -0.41 |
550-600 | 140 | 0.22 | 0.31 | 1.08 | -0.58 |
600-650 | 140 | 0.23 | 0.26 | 0.85 | -0.28 |
650-700 | 140 | 0.18 | 0.27 | 0.84 | -0.42 |
700-750 | 140 | 0.11 | 0.26 | 0.74 | -0.35 |
750-800 | 134 | 0.06 | 0.28 | 0.78 | -0.33 |
800-850 | 127 | 0.07 | 0.27 | 0.71 | -0.32 |
850-900 | 80 | 0.10 | 0.28 | 0.83 | -0.40 |
900-950 | 1 | 0.15 | 0.00 | 0.15 | 0.15 |
950-1000 | 0 | - | - | - | - |
Error data: 0 of 825
On land: 0 of 25
Invalid position: 0 of 25
Error data (low): 0 of 825
Error data (high): 0 of 825
Error data: 0 of 825
◊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 |