served from IRI/LDEO Climate Data Library

*Longitude*(longitude)- grid: /X (degree_east) periodic (0.5E) to (0.5W) by 1.0 N= 360 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered [ (60.5S) (59.48S) (58.46005S) ... (60.5N)] N= 129 pts :grid
*Depth*- grid: /Z (m) ordered [ (3990.95) (3254.05) (2543.45) (1900.045) (1349.125) (906.96) (579.125) (360.03) (233.44) (174.055) (150.0) (135.0) (120.0) (105.0) (90.0) (75.0) (60.0) (45.0) (30.0) (15.0) (0.0)] :grid

*bufferwordsize*- 8
*CE*- null
*CS*- null
*datatype*- doublearraytype
*file_missing_value*- -9.98999971E33
*gridid*- 170616864
*missing_value*- NaN
*pointwidth*- 1.0
*standard_name*- time
*units*- 30.1592894744621 degree_Kelvin meter radian north year
^{-3} *history*- mean $partialdiff sub T$ detrended-bfl $partialdiff sub T$ $partialdiff sub T$ $integral dY$ detrended-bfl $integral dZ$ [ UMD Carton goa beta7 t ]
- beta7 run with 16 level data assimilation (altimetry 14 level), 50-2000

Averaged over T[Mar 1950, Oct 2001] minimum 0.0% data present

- beta7 run with 16 level data assimilation (altimetry 14 level), 50-2000

Carton, J.A., G. Chepurin, and X. Cao, 2000b: A Simple Ocean Data Assimilation analysis of the global upper ocean 1950-1995 Part 2: results, J. Phys. Oceanogr., 30, 311-326

Last updated: *Thu, 23 Jan 2003 21:17:59 GMT*

X | Y | Z | |

mean $partialdiff sub T$ detrended-bfl $partialdiff sub T$ $partialdiff sub T$ $integral dY$ detrended-bfl $integral dZ$ [ UMD Carton goa beta7 t ] [ 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