served from IRI/LDEO Climate Data Library

*Time*- grid: /T (months since 1960-01-01) ordered (Jan 1960) to (Dec 1960) by 1.0 N= 12 pts :grid
*Longitude*- grid: /X (degree_east) ordered (0) to (0) by 1.0 N= 361 pts :grid
*Latitude*- grid: /Y (degree_north) ordered (90S) to (90N) by 1.0 N= 181 pts :grid
*Depth*- grid: /Z (m) ordered [ (5.0) (15.0) (25.0) (40.0) (62.5) (87.5) (112.5) (137.5) (175.0) (225.0) (275.0) (350.0) (450.0) (550.0) (650.0) (750.0) (850.0) (950.0)] :grid

*CE*- null
*CS*- null
*datatype*- realarraytype
*missing_value*- NaN
*units*- 0.000304617419786708 degree_Kelvin meter
^{-1}radian^{2}east *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: *Fri, 18 Sep 2015 18:39:07 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