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GTSPP Data Product Centre for the North Pacific Region hosted by the Japan Meteorological Agency

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Ship Observations Team (SOT)

NORTHEWEST SANDERLING(VNVZ), PX11
Observation period : 2016/10/23 to 2016/10/29

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 profiles	Number of data	AVE	RMSD	MAXD	MIND
34	6384	-0.04	0.88	2.97	-4.10

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 range	Number of data	AVE	RMSD	MAXD	MIND
0-50	500	-0.11	0.46	0.38	-2.19
50-100	500	-0.63	1.04	1.62	-4.10
100-150	500	-0.73	1.35	2.27	-4.09
150-200	500	-0.67	1.36	2.97	-3.57
200-250	500	-0.09	1.04	2.18	-2.31
250-300	500	0.47	0.85	2.43	-1.23
300-350	500	0.42	0.62	1.62	-0.99
350-400	500	0.35	0.51	1.43	-0.88
400-450	500	0.15	0.47	1.13	-1.07
450-500	500	0.12	0.39	1.29	-0.75
500-550	200	0.11	0.35	1.18	-0.61
550-600	200	0.11	0.32	0.87	-0.50
600-650	200	0.10	0.27	0.73	-0.35
650-700	195	0.08	0.23	0.78	-0.35
700-750	179	0.04	0.20	0.46	-0.39
750-800	169	0.04	0.23	0.55	-0.59
800-850	157	0.03	0.22	0.33	-0.59
850-900	78	0.07	0.18	0.40	-0.28
900-950	6	0.27	0.12	0.45	0.18
950-1000	0	-	-	-	-

Results of QC

A total of 34 profiles (1150 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 1150

Position on land test

On land: 0 of 34

Invalid position: 0 of 34

Regional range test

Error data (low): 0 of 1150

Error data (high): 0 of 1150

Gradient test

Error data: 0 of 1150

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

Summary of QC

No errors were detected with JMA's quality control procedures.
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 9°N. It's to be noted that the results of assimilation is considered to be less accurate in the marginal seas.
There was no significant bias 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.

◊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