served from IRI/LDEO Climate Data Library

*Time*(time)- grid: /T (months since 1960-01-01) ordered (0000 1 Sep 1960) to (0000 1 Sep 1961) by 1.0 N= 13 pts :grid
*Longitude*(longitude)- grid: /X (degree_east) ordered (0) to (0) by 4.0 N= 91 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered (59.5S) to (59.5N) by 1.0 N= 120 pts :grid

*bufferwordsize*- 8
*CE*- null
*CS*- null
*datatype*- doublearraytype
*missing_value*- NaN
*units*- 1.01002850231153×10
^{-07}meter radian east year^{3} *history*- detrended-bfl $integral dT$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- Monthly mean sea surface height anomaly.
**USA**

$integral dT$ [ detrended-bfl $integral dT$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl ( IGOSS TOPEX NOAA ssha ) climatology ]- Averaged over T2[Sep 1992 - Aug 1993, Sep 2001 - Aug 2002] minimum 0.0% data present

- Monthly mean sea surface height anomaly.

Last updated: *Tue, 19 May 2015 19:52:55 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 T
- Differentiate along X Y T
- Take differences along X Y T

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

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

Maximum over X Y T | X Y X T Y T | X Y T |

Minimum over X Y T | X Y X T Y T | X Y T |

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

Note on units