served from IRI/LDEO Climate Data Library

*Longitude*- grid: /X (degree_east) periodic (1E) to (0) 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 [ (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

*CE*- null
*CS*- null
*datatype*- realarraytype
*missing_value*- NaN
*units*- degree_Celsius
*standard units**- degree_Kelvin
*history*- $partialdiff sub Y$ detrended-bfl mean $integral dY$ detrended-bfl [ LEVITUS94 MONTHLY temp ]
- World Ocean Atlas CD-ROM, Levitus et al., 1994

Averaged over T[Jan, Dec] minimum 0.0% data present

- 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*

X | Y | Z | |

$partialdiff sub Y$ detrended-bfl mean $integral dY$ detrended-bfl [ LEVITUS94 MONTHLY temp ] [ X Y Z |] | 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
- 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