served from IRI/LDEO Climate Data Library

*Time*(time)- grid: /T (months since 1960-01-01) ordered (Jan 1981) to (Jan 1990) by 1.0 N= 109 pts :grid
*Longitude*(longitude)- grid: /X (degree_east) ordered (101W) to (21E) by 2.0 N= 62 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered (35S) to (57N) by 2.0 N= 47 pts :grid

*CE*- null
*CS*- null
*datatype*- realarraytype
*units*- dynes /cm
^{2} *standard units**- 0.1 kilogram meter
^{-1}second^{-2} *history*- $partialdiff sub Y$ detrended-bfl $integral dY$ detrended-bfl detrended-bfl $integral dY$ [ Morliere taux ]

Wind stresses from Alain Morliere's model.

- $partialdiff sub Y$ detrended-bfl $integral dY$ detrended-bfl detrended-bfl $integral dY$ [ Morliere taux ] climatology
- Wind stresses from Alain Morliere's model.

Averaged over T2[1981, 1989]

- Wind stresses from Alain Morliere's model.

- $partialdiff sub Y$ detrended-bfl $integral dY$ detrended-bfl detrended-bfl $integral dY$ [ Morliere taux ]

Last updated: *Mon, 12 Sep 2016 21:27:18 GMT*

T | X | Y | |

$partialdiff sub Y$ [ $partialdiff sub Y$ detrended-bfl $integral dY$ detrended-bfl detrended-bfl $integral dY$ ( Morliere taux ) anomalies ][ 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