served from IRI/LDEO Climate Data Library

*Time*- grid: /T (months since 01-Jan) periodic (Jan) to (Dec) by 1.0 N= 12 pts :grid
*Longitude*- grid: /X (degree_east) ordered (1E) to (1W) by 1.0 N= 359 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

*datatype*- realarraytype
*missing_value*- NaN
*units*- 687.549354156988 degree_Kelvin radian
^{-1}east year^{-1} *history*- $partialdiff sub X$ $partialdiff sub T$ $partialdiff sub X$ max $integral dX$ [ LEVITUS94 MONTHLY temp ]
- World Ocean Atlas CD-ROM, Levitus et al., 1994

max over Y[89.5S, 89.5N]

- World Ocean Atlas CD-ROM, Levitus et al., 1994

Levitus_Boyer1994a

Levitus_etal1994

Levitus_Boyer1994c

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

T | X | Z | |

$partialdiff sub X$ $partialdiff sub T$ $partialdiff sub X$ max $integral dX$ [ LEVITUS94 MONTHLY temp ] [ X Z | T] | 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 Z T
- Differentiate along X Z T
- Take differences along X Z T

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

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

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

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

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

Note on units