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) to (1.875W) by 1.875 N= 192 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered [ (90N) (88.572N) (86.723N) (84.862N) (82.999N) (81.135N) (79.271N) (77.406N) (75.541N) (73.676N) (71.811N) (69.946N) (68.081N) (66.216N) (64.351N) (62.486N) (60.62N) (58.755N) (56.89N) (55.025N) (53.16N) (51.294N) (49.429N) (47.564N) (45.699N) (43.833N) (41.968N) (40.103N) (38.238N) (36.372N) (34.507N) (32.642N) (30.777N) (28.911N) (27.046N) (25.181N) (23.316N) (21.45N) (19.585N) (17.72N) (15.855N) (13.989N) (12.124N) (10.259N) (8.393997N) (6.528N) (4.663002N) (2.797997N) (0.9329987N) (0.9329987S) (2.797997S) (4.663002S) (6.528S) (8.393997S) (10.259S) (12.124S) (13.989S) (15.855S) (17.72S) (19.585S) (21.45S) (23.316S) (25.181S) (27.046S) (28.911S) (30.777S) (32.642S) (34.507S) (36.372S) (38.23801S) (40.103S) (41.968S) (43.83299S) (45.69901S) (47.564S) (49.429S) (51.29401S) (53.16S) (55.02499S) (56.89S) (58.755S) (60.62S) (62.48599S) (64.351S) (66.216S) (68.08099S) (69.946S) (71.811S) (73.67599S) (75.541S) (77.40601S) (79.271S)] :grid
*Depth*- grid: /Z (m) ordered [ (12.5) (37.5) (62.5) (87.5) (112.5) (137.5) (162.5) (187.5) (212.5) (237.5) (262.5) (287.5) (313.523) (344.632) (387.805) (450.677) (540.282)] :grid

*bufferwordsize*- 4
*datatype*- realarraytype
*missing_value*- 9999
*pointwidth*- 1.0
*units*- Celsius_scale
*standard units**- degree_Kelvin above 273.15

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 temp[ 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