served from IRI/LDEO Climate Data Library
NOAA NCEP EMC CMB Pacific weekly D20eq: Depth of 20C data
weekly D20eq Depth of 20C from NOAA NCEP EMC CMB Pacific: Pacific Ocean Hindcast data derived from a model-based ocean analysis system.Independent Variables (Grids)
- Time
- grid: /T (julian_day) unordered [ (0000 5 Jan 1997) (0000 12 Jan 1997) (0000 19 Jan 1997) ... (0000 26 Oct 2008)] N= 812 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (122.25E) to (71.25W) by 1.5 N= 112 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered [ (0)] :grid
Other Info
- CE
- 200
- CS
- 0
- datatype
- realarraytype
- gridid
- 171065320
- maxncolor
- 254
- missing_value
- NaN
- positive
- down
- units
- m
- standard units*
- meter
- history
- NOAA NCEP EMC CMB Pacific weekly D20eq
- toS: regridded Z to NOAA NCEP EMC CMB Pacific weekly temp 0
T: 6-12 Feb 2005 to 1200 29 Oct 2008 appended from NOAA NCEP EMC CMB Pacific godas D20eq
- toS: regridded Z to NOAA NCEP EMC CMB Pacific weekly temp 0
- colorscale
References
Behringer, D. W., M. Ji, and A. Leetmaa, 1998: An Improved coupled model for ENSO prediction and implications for ocean initialization. Part I: The ocean data assimilation system. Mon. Wea. Rev., 126, 1013-1021.Ji, M., A. Leetmaa, and J. Derber, 1995: An ocean analysis system for seasonal to interannual climate studies. Mon. Wea. Rev., 123, 460-481.
Ji, M., and T. M. Smith, 1995: Ocean model response to temperature data and varying surface wind stress: Intercomparisons and Implications for climate forecast. Mon. Wea. Rev., 123, 1811-1821.
Last updated: Wed, 13 Feb 2019 20:27:28 GMT
Data Views
Views
data as colors
data as contours| T | X | Y | |
 NOAA NCEP EMC CMB Pacific weekly D20eq 0[ X | Y T] | M | M | M |
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Filters
Here are some filters that are useful for manipulating data. There are actually many more available, but they have to be entered manually. See Ingrid Function Documentation for more information.- 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 T
- Differentiate along X T
- Take differences along X T
RMS (root mean square with mean *not* removed) over X T | X T |
RMSA (root mean square with mean removed) over X T | X T |
Maximum over X T | X T |
Minimum over X T | X T |
Detrend (best-fit-line) over X T | X T |
Note on units