Number of profiles | Number of data | AVE | RMSD | MAXD | MIND |
---|---|---|---|---|---|
17 | 5002 | 0.07 | 0.58 | 3.04 | -2.65 |
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 | 0.12 | 0.32 | 0.80 | -0.91 |
50-100 | 400 | -0.02 | 0.59 | 1.95 | -2.05 |
100-150 | 400 | 0.11 | 0.82 | 2.74 | -2.52 |
150-200 | 400 | -0.12 | 0.97 | 2.56 | -2.65 |
200-250 | 400 | 0.04 | 0.83 | 3.04 | -1.55 |
250-300 | 400 | 0.11 | 0.57 | 1.94 | -0.93 |
300-350 | 383 | 0.18 | 0.54 | 1.73 | -0.73 |
350-400 | 375 | 0.12 | 0.52 | 1.16 | -0.94 |
400-450 | 375 | 0.08 | 0.47 | 0.92 | -0.72 |
450-500 | 375 | 0.08 | 0.35 | 0.73 | -0.50 |
500-550 | 145 | 0.07 | 0.30 | 0.68 | -0.43 |
550-600 | 140 | 0.09 | 0.29 | 0.62 | -0.47 |
600-650 | 140 | 0.07 | 0.28 | 0.56 | -0.53 |
650-700 | 140 | 0.04 | 0.27 | 0.52 | -0.55 |
700-750 | 140 | 0.08 | 0.24 | 0.50 | -0.43 |
750-800 | 137 | 0.08 | 0.21 | 0.47 | -0.36 |
800-850 | 130 | 0.07 | 0.19 | 0.44 | -0.35 |
850-900 | 94 | 0.05 | 0.19 | 0.42 | -0.31 |
900-950 | 3 | 0.13 | 0.40 | 0.41 | -0.43 |
950-1000 | 0 | - | - | - | - |
Error data: 0 of 552
On land: 0 of 17
Invalid position: 0 of 17
Error data (low): 0 of 552
Error data (high): 0 of 552
Error data: 0 of 552
◊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 |