served from IRI/LDEO Climate Data Library

*Time*- grid: /T (months since 1960-01-01) ordered (16 Dec 1959 - 15 Jan 1960) to (16 Nov 1960 - 15 Dec 1960) by 1.0 N= 12 pts :grid
*Longitude*- grid: /X (degree_east) periodic (0.5E) to (0.5W) by 1.0 N= 360 pts :grid
*Latitude*- grid: /Y (degree_north) ordered (89S) to (89N) by 1.0 N= 179 pts :grid
*Depth*- grid: /Z (m) ordered [ (0.0) (10.0) (20.0) (32.5) (51.25) (75.0) (100.0) (125.0) (156.25) (200.0) (250.0) (312.5) (400.0) (500.0) (600.0) (700.0) (800.0) (900.0) (1000.0)] :grid

*CE*- null
*CS*- null
*datatype*- realarraytype
*missing_value*- NaN
*units*- 687.549354156988 degree_Kelvin radian
^{-1}north year^{-1} *history*- World Ocean Atlas CD-ROM, Levitus et al., 1994

S. Levitus, T.P. Boyer. World Ocean Atlas 1994 Volume 2: Oxygen, number 2, 1994

S. Levitus, R. Burgett, T.P. Boyer. World Ocean Atlas 1994 Volume 3: Nutrients, number 3, 1994

S. Levitus, T.P. Boyer. World Ocean Atlas 1994 Volume 4: Temperature, number 4, 1994

Last updated: *Wed, 13 Feb 2019 20:27:28 GMT*

- 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