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

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The last 30 days SOOP observation

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Ship Observations Team (SOT)

KEIFU-MARU(JPBN), PX46
Observation period : 2014/7/22 to 2014/8/15

This page shows results for the PX46 line based on monitoring by the KEIFU-MARU and comparison with the result of assimilation by MOVE-NP.

Overall statistics

Number of profiles	Number of data	AVE	RMSD	MAXD	MIND
48	14391	0.00	0.50	2.76	-4.06

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	1025	-0.09	0.67	1.94	-3.42
50-100	1025	-0.16	0.69	1.54	-1.90
100-150	1025	-0.02	0.95	2.64	-1.90
150-200	1025	-0.09	0.81	2.76	-4.00
200-250	1025	-0.26	0.47	0.93	-4.06
250-300	1025	0.01	0.35	0.94	-1.69
300-350	1025	0.05	0.31	0.90	-0.97
350-400	1025	0.06	0.28	0.88	-0.79
400-450	1025	0.06	0.28	0.88	-0.51
450-500	1025	0.08	0.20	0.98	-0.69
500-550	410	0.09	0.31	1.54	-0.84
550-600	410	0.06	0.33	1.62	-0.74
600-650	410	0.04	0.26	1.81	-0.61
650-700	410	0.06	0.20	1.48	-0.54
700-750	410	0.09	0.17	0.86	-0.45
750-800	410	0.12	0.14	0.81	-0.22
800-850	410	0.16	0.12	0.60	-0.17
850-900	410	0.15	0.12	0.45	-0.16
900-950	410	0.12	0.11	0.45	-0.23
950-1000	410	0.08	0.03	0.39	-0.30

Results of QC

A total of 48 profiles (1053 data, reported by BATHY or TESAC) were received from the KEIFU-MARU.
The results of JMA quality control are as follows.

Grounded test

Error data: 0 of 1053

Position on land test

On land: 0 of 48

Invalid position: 0 of 48

Regional range test

Error data (low): 0 of 1053

Error data (high): 0 of 1053

Gradient test

Error data: 0 of 1053

For datails 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 3°C between observation data and the results of assimilation at around 2°S at a depth of around 200 m.
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 PX46 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