Number of profiles | Number of data | AVE | RMSD | MAXD | MIND |
---|---|---|---|---|---|
15 | 4484 | 0.12 | 0.59 | 2.14 | -2.09 |
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 | 375 | -0.01 | 0.36 | 1.45 | -0.94 |
50-100 | 375 | 0.45 | 0.60 | 2.14 | -1.08 |
100-150 | 367 | 0.04 | 0.83 | 2.08 | -1.99 |
150-200 | 350 | -0.23 | 0.85 | 1.46 | -2.09 |
200-250 | 350 | -0.08 | 0.74 | 1.54 | -1.90 |
250-300 | 350 | 0.21 | 0.61 | 1.39 | -1.48 |
300-350 | 350 | 0.26 | 0.59 | 1.43 | -1.27 |
350-400 | 350 | 0.24 | 0.53 | 1.37 | -0.58 |
400-450 | 350 | 0.17 | 0.43 | 1.08 | -0.44 |
450-500 | 334 | 0.19 | 0.35 | 1.02 | -0.41 |
500-550 | 130 | 0.17 | 0.33 | 0.88 | -0.49 |
550-600 | 130 | 0.19 | 0.28 | 0.94 | -0.30 |
600-650 | 128 | 0.19 | 0.33 | 1.15 | -0.42 |
650-700 | 120 | 0.12 | 0.33 | 0.68 | -0.68 |
700-750 | 116 | 0.11 | 0.33 | 0.74 | -0.76 |
750-800 | 110 | 0.07 | 0.31 | 0.54 | -0.75 |
800-850 | 108 | 0.02 | 0.28 | 0.43 | -0.70 |
850-900 | 89 | 0.00 | 0.26 | 0.38 | -0.66 |
900-950 | 2 | 0.25 | 0.15 | 0.40 | 0.11 |
950-1000 | 0 | - | - | - | - |
Error data: 0 of 505
On land: 0 of 15
Invalid position: 0 of 15
Error data (low): 0 of 505
Error data (high): 0 of 505
Error data: 0 of 505
◊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 |