NORTHEWEST SANDERLING(VNVZ), PX11
Observation period : 2016/12/15 to 2016/12/22

This page shows results for the PX11 line based on monitoring by the NORTHEWEST SANDERLING and comparison with the result of assimilation by MOVE-NP.

Overall statistics

Number of profilesNumber of dataAVERMSDMAXDMIND
4363570.040.874.61-4.08

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



Statistics for each depth range

Depth rangeNumber of dataAVERMSDMAXDMIND
0-50648-0.100.524.16-1.96
50-100625-0.291.093.43-4.04
100-150581-0.141.464.61-4.08
150-2005510.251.444.11-2.61
200-2505250.291.103.17-1.77
250-3005090.240.772.59-1.36
300-3504750.100.551.45-1.12
350-4004590.050.411.38-1.07
400-450450-0.000.270.52-0.76
450-500439-0.060.320.54-0.80
500-5501700.040.280.69-0.66
550-6001700.090.320.74-0.70
600-6501650.110.370.81-0.69
650-7001480.110.320.86-0.60
700-7501360.110.290.63-0.53
750-8001110.110.260.65-0.45
800-8501010.110.240.54-0.42
850-900820.060.220.52-0.32
900-950120.060.170.30-0.24
950-10000----


Results of QC

A total of 43 profiles (1374 data, reported by BATHY or TESAC) were received from the NORTHEWEST SANDERLING.
The results of JMA quality control are as follows.
  • Grounded test
  • Error data: 0 of 1374

  • Position on land test
  • On land: 0 of 43

    Invalid position: 0 of 43

  • Regional range test
  • Error data (low): 0 of 1374

    Error data (high): 4 of 1374

  • Gradient test
  • Error data: 0 of 1374

For details of JMA's quality control procedures, please refer to this page.


Summary of QC

  • Some erroneous profiles are detected by JMA's automated quality control procedures. These are checked by the regional range test.
  • There were differences above 2°C between the results of assimilation and a profile data observed at depths of between 50 and 300m in the seas south from 10°N. It's to be noted that the results of assimilation is considered to be less accurate in the marginal seas.
  • With the exception of the above errors and differences, there were no significant biases in comparison with the results of assimilation by JMA.


Figures

◊Station map ◊Vertical temperature profile

Vertical profile of temperature along the observing line of PX11 moved the entire profile by 5 degree Celsius.

station map water fall
◊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.

observation scatter plot (summary of all station)
◊Vertical sections for the result of assimilation by MOVE-NP ◊Distribution of differences (Obs. - Assim.) by depth
result of assimilation scatter plot(depth bases)
◊Vertical sections of differences (Obs. - Assim.) ◊Distribution of differences (Obs. - Assim.) by temperature
differences (Obs. - Assim.) scatter plot (tempereture basis)