served from IRI/LDEO Climate Data Library

*Time*- grid: /T (months since 01-Jan) ordered (Jan) to (Jan) by 1.0 N= 13 pts :grid
*Longitude*- grid: /X (degree_east) ordered (0) to (0) by 1.0 N= 361 pts :grid
*Latitude*- grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 1.0 N= 180 pts :grid
*Depth*- grid: /Z (m) ordered [ (0.0) (10.0) (20.0) (30.0) (50.0) (75.0) (100.0) (125.0) (150.0) (200.0) (250.0) (300.0) (400.0) (500.0) (600.0) (700.0) (800.0) (900.0) (1000.0)] :grid

*bufferwordsize*- 8
*CE*- null
*CS*- null
*datatype*- doublearraytype
*missing_value*- NaN
*units*- 0.00145444104332861 degree_Kelvin radian east year
*history*- World Ocean Atlas CD-ROM, Levitus et al., 1994

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

T | X | Y | Z | |

$integral dT$ $integral dX$ [ LEVITUS94 MONTHLY 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