served from IRI/LDEO Climate Data Library

*Time*(time)- grid: /T (months since 01-Jan) periodic (Nov) to (Oct) by 1.0 N= 12 pts :grid
*Longitude*(longitude)- grid: /X (degree_east) ordered (178.5W) to (178.5E) by 1.0 N= 358 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered (90.5S) to (90.5N) by 1.0 N= 182 pts :grid

*bufferwordsize*- 8
*CE*- null
*colorscalename*- sstacolorscale
*CS*- null
*datatype*- doublearraytype
*maxncolor*- 254
*PLOTCOAST*- 1
*units*- 5.3165769342078×10
^{-06}degree_Kelvin radian^{3}north *history*- IGOSS nmc Reyn_SmithOIv1 monthly ssta
- Monthly mean sea surface temperature anomaly (blended from ship, buoy, and bias-corrected satellite data)

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

Last updated: *Mon, 12 Sep 2016 21:14:59 GMT*

T | X | Y | |

$integral dY$ $partialdiff sub X$ $integral dX$ detrended-bfl $integral dY$ detrended-bfl $integral dX$ [ IGOSS nmc Reyn_SmithOIv1 monthly ssta climatology ] [ X Y T |] | 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 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