served from IRI/LDEO Climate Data Library

*Pressure*- grid: /P (mb) ordered [ (1000) (925) (850) (700) (600) (500) (400) (300) (250) (200) (150) (100) (70) (50) (30) (20) (10)] :grid
*Time*(time)- grid: /T (months since 1960-01-01) ordered (Jan 1949) to (Feb 2023) by 1.0 N= 890 pts :grid
*Longitude*(longitude)- grid: /X (degree_east) periodic (0) to (2.5W) by 2.5 N= 144 pts :grid
*Latitude*(latitude)- grid: /Y (degree_north) ordered (90N) to (90S) by 2.5 N= 73 pts :grid

*bufferwordsize*- 4
*calendar*- standard
*center*- US Weather Service - National Met. Center
*datatype*- realarraytype
*grib_name*- UGRD
*gribfield*- 1
*GRIBgridcode*- 2
*gribleveltype*- 100
*gribNumBits*- 12
*gribparam*- 33
*gribvariable*- 33
*missing_value*- 9.99900026E20
*PDS_TimeRange*- 113
*pointwidth*- 1.0
*process*- 62 wave triangular, 28 layer Spectral model from "Medium Range Forecast" run
*PTVersion*- 2
*scale_max*- 124.4
*scale_min*- -66.379997
*subcenter*- NCEP Ensemble Products
*units*- m /s
*standard units**- meter second
^{-1}

Last updated: *Thu, 02 Mar 2023 21:51:41 GMT*

Expires: *Mon, 03 Apr 2023 00:00:00 GMT*

P | T | X | Y | |

NOAA NCEP-NCAR CDAS-1 MONTHLY Intrinsic PressureLevel u[ X Y | P T] | 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 P T
- Differentiate along X Y P T
- Take differences along X Y P T

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

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

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

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

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

Note on units