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) periodic (1E) to (0) 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 [ (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*- degree_Kelvin meter
^{-1} *history*- 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 | Y | Z | |

$partialdiff sub Y$ detrended-bfl $integral dY$ $partialdiff sub Z$ detrended-bfl [ 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