served from IRI/LDEO Climate Data Library

*Time*(time)- grid: /T (months since 1960-01-01) ordered (Nov 1960) to (Oct 1961) by 1.0 N= 12 pts :grid
*Longitude*(longitude)- grid: /X (degree_east) ordered (178.5E) to (178.5W) by 1.0 N= 364 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 1.0 N= 180 pts :grid

*bufferwordsize*- 8
*CE*- null
*colorscalename*- sstacolorscale
*CS*- null
*datatype*- doublearraytype
*maxncolor*- 254
*PLOTCOAST*- 1
*units*- 1.61952194779591×10
^{-09}degree_Kelvin radian^{5}east *history*- IGOSS nmc Reyn_SmithOIv1 monthly ssta
- Monthly mean sea surface temperature anomaly (blended from ship, buoy, and bias-corrected satellite data)

$integral dX$ detrended-bfl $integral dX$ $partialdiff sub T$ detrended-bfl $integral dX$ $integral dY$ detrended-bfl $integral dX$ $integral dT$ detrended-bfl [ IGOSS nmc Reyn_SmithOIv1 monthly ssta climatology ]- Averaged over T2[Nov 1981 - Oct 1982, Nov 2001 - Oct 2002]

Last updated: *Wed, 13 Feb 2019 20:27:28 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