Number of profiles | Number of data | AVE | RMSD | MAXD | MIND |
---|---|---|---|---|---|
27 | 3723 | -0.07 | 0.82 | 3.28 | -4.67 |
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 | 357 | 0.19 | 0.38 | 1.19 | -2.44 |
50-100 | 350 | -0.91 | 1.26 | 1.21 | -4.67 |
100-150 | 333 | -0.61 | 1.19 | 2.85 | -3.50 |
150-200 | 306 | 0.19 | 1.03 | 3.28 | -1.73 |
200-250 | 286 | -0.03 | 0.79 | 1.74 | -1.81 |
250-300 | 275 | 0.05 | 0.66 | 1.41 | -1.15 |
300-350 | 275 | 0.09 | 0.61 | 1.10 | -0.90 |
350-400 | 275 | 0.07 | 0.59 | 1.29 | -0.77 |
400-450 | 260 | 0.07 | 0.50 | 1.06 | -0.64 |
450-500 | 250 | 0.07 | 0.38 | 1.03 | -0.52 |
500-550 | 100 | 0.12 | 0.35 | 0.90 | -0.42 |
550-600 | 100 | 0.11 | 0.39 | 0.99 | -0.52 |
600-650 | 100 | 0.12 | 0.39 | 1.06 | -0.46 |
650-700 | 100 | 0.06 | 0.36 | 1.00 | -0.34 |
700-750 | 100 | 0.03 | 0.36 | 1.05 | -0.34 |
750-800 | 99 | 0.01 | 0.29 | 0.85 | -0.35 |
800-850 | 82 | 0.04 | 0.24 | 0.64 | -0.27 |
850-900 | 69 | 0.07 | 0.18 | 0.39 | -0.18 |
900-950 | 6 | 0.14 | 0.08 | 0.28 | 0.03 |
950-1000 | 0 | - | - | - | - |
Error data: 0 of 900
On land: 0 of 27
Invalid position: 0 of 27
Error data (low): 0 of 900
Error data (high): 2 of 900
Error data: 0 of 900
◊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 |