served from IRI/LDEO Climate Data Library

*Time*(time)- grid: /T (months since 1960-01-01) ordered (Jan 1982) to (May 2014) by 1.0 N= 389 pts :grid
*Longitude*(longitude)- grid: /X (degree_east) periodic (0.9375E) to (0.9375W) by 1.875 N= 192 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered [ (89.286N) (87.647N) (85.792N) (83.93N) (82.067N) (80.203N) (78.338N) (76.473N) (74.609N) (72.744N) (70.879N) (69.014N) (67.148N) (65.283N) (63.418N) (61.553N) (59.688N) (57.823N) (55.957N) (54.092N) (52.227N) (50.362N) (48.497N) (46.631N) (44.766N) (42.901N) (41.036N) (39.17N) (37.305N) (35.44N) (33.575N) (31.709N) (29.844N) (27.979N) (26.114N) (24.248N) (22.383N) (20.518N) (18.653N) (16.787N) (14.922N) (13.057N) (11.192N) (9.325996N) (7.460999N) (5.596001N) (3.731003N) (1.864998N) (0) (1.864998S) (3.731003S) (5.596001S) (7.460999S) (9.325996S) (11.192S) (13.057S) (14.922S) (16.787S) (18.653S) (20.518S) (22.383S) (24.248S) (26.114S) (27.979S) (29.844S) (31.709S) (33.575S) (35.44S) (37.305S) (39.17S) (41.036S) (42.901S) (44.76601S) (46.631S) (48.49699S) (50.362S) (52.22701S) (54.092S) (55.957S) (57.823S) (59.688S) (61.55299S) (63.418S) (65.283S) (67.14799S) (69.01401S) (70.879S) (72.744S) (74.60899S) (76.47301S) (78.338S) (80.2S)] :grid
*Depth*- grid: /Z (m) ordered [ (0.0) (25.0) (50.0) (75.0) (100.0) (125.0) (150.0) (175.0) (200.0) (225.0) (250.0) (275.0) (300.0) (327.047) (362.218) (413.392) (487.961)] :grid

*bufferwordsize*- 4
*datatype*- realarraytype
*missing_value*- 9999
*pointwidth*- 1.0
*units*- m /s
*standard units**- meter second
^{-1}

Yimin Liu, Weijing Li, Peiqun Zhang, 2005, NCC 4-Dimensional Ocean Data Assimilation System and the Studies on Its Results in the Middle Pacific, ACTA Oceanologica Sinica (in Chinese), Vol.27, No.1,27-35.

Last updated: *Wed, 06 Jan 2021 14:52:06 GMT*

T | X | Y | Z | |

CMA BCC GODAS u[ X Y | Z T] | M | M | M | M |
---|

- Monthly Climatology calculates a monthly climatology by averaging over all years.
- anomalies calculates the difference between the (above) monthly climatology and the original data.
- Integrate along X Y Z T
- Differentiate along X Y Z T
- Take differences along X Y Z T

RMS (root mean square with mean *not* removed) over X Y Z T | X Y X Z X T Y Z Y T Z T | X Y Z X Y T X Z T Y Z T | X Y Z T |

RMSA (root mean square with mean removed) over X Y Z T | X Y X Z X T Y Z Y T Z T | X Y Z X Y T X Z T Y Z T | X Y Z T |

Maximum over X Y Z T | X Y X Z X T Y Z Y T Z T | X Y Z X Y T X Z T Y Z T | X Y Z T |

Minimum over X Y Z T | X Y X Z X T Y Z Y T Z T | X Y Z X Y T X Z T Y Z T | X Y Z T |

Detrend (best-fit-line) over X Y Z T | X Y X Z X T Y Z Y T Z T | X Y Z X Y T X Z T Y Z T | X Y Z T |

Note on units