served from IRI/LDEO Climate Data Library

*Longitude*- grid: /X (degree_east) ordered (0.5E) to (0.5W) by 1.0 N= 360 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 [ (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)] :grid

*CE*- null
*CS*- null
*datatype*- realarraytype
*missing_value*- NaN
*units*- 12 degree_Kelvin meter
^{-2}year^{-1} *history*- $partialdiff sub X$ max $integral dX$ detrended-bfl $partialdiff sub T$ detrended-bfl $partialdiff sub Z$ detrended-bfl detrended-bfl $partialdiff sub Z$ [ LEVITUS94 MONTHLY temp ]
- World Ocean Atlas CD-ROM, Levitus et al., 1994

max over T[16 Dec - 15 Jan, 16 Nov - 15 Dec]

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

Levitus_Boyer1994a

Levitus_etal1994

Levitus_Boyer1994c

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
- Differentiate along X Y Z
- Take differences along X Y Z

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

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

Maximum over X Y Z | X Y X Z Y Z | X Y Z |

Minimum over X Y Z | X Y X Z Y Z | X Y Z |

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

Note on units