served from IRI/LDEO Climate Data Library

*depth*- grid: /depth (m) ordered [ (0.0)] :grid
*time*- grid: /time (months since 1960-01-01) ordered (Jan 1977) to (Oct 2014) by 1.0 N= 454 pts :grid
*Longitude*- grid: /X (degree_east) ordered [ (130E) (137E) (143E) (147E) (154E) (155E) (156E) (158E) (161E) (165E) (167E) (168E) (170E) (180) (176W) (170W) (157W) (155W) (147W) (140W) (137W) (132W) (125W) (110W) (95W)] :grid
*Latitude*- grid: /Y (degree_north) ordered [ (8.5S) (7.5S) (6.5S) (5.5S) (4.5S) (3.5S) (2.5S) (1.5S) (0.5S) (0.5N) (1.5N) (2.5N) (3.25N) (4.25N) (5.5N) (6.5N) (7.5N) (8.5N) (9.5N) (10.5N) (11.5N)] :grid

*CE*- 10
*CI*- 1
*CS*- -10
*CSCALE*- 0.035
*datatype*- realarraytype
*epic_code*- 423
*file_missing_value*- 1.00000004E35
*FORTRAN_format*- F9.4
*generic_name*- v
*missing_value*- NaN
*units*- 57.2957795130823 meter radian
^{-1}north second^{-1} *history*- [(Mean surface wind vectors (m/s) and sea surface temperature (C) as well as anomalies in the tropical Pacific.) (COADS Wind and Reynold-Smith (1994) climatologies.) (
**USA-FRANCE-JAPAN-KOREA-TAIWAN**)]

Soreide_etal1994

Last updated: *Mon, 16 Feb 2015 21:51:22 GMT*

depth | time | X | Y | |

$partialdiff sub Y$ [ IGOSS TOGA-TAO.cdf va ] 0.0 m[ X Y depth | time] | M | 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 time
- Differentiate along X Y time
- Take differences along X Y time

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

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

Maximum over X Y time | X Y X time Y time | X Y time |

Minimum over X Y time | X Y X time Y time | X Y time |

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

Note on units