served from data-library.gov.ls
root mean sq anom ∂X [ NOAA NCDC ERSST version3b anom ] : ∂X Extended reconstructed SST anomalies data
anom partial_X partial_X ∂X Extended reconstructed SST anomalies from NOAA NCDC ERSST version3b: ERSST.v3b: Extended Reconstructed Sea Surface Temperature Dataset, Verson 3b.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 1960-01-01) ordered (16 Jan 1854 - 15 Feb 1854) to (16 Jan 2020 - 15 Feb 2020) by 1.0 N= 1993 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (88S) to (88N) by 2.0 N= 89 pts :grid
- zlev
- grid: /zlev (meters) ordered [ (0.0)] :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- -999.0
- iridl:hasSemantics
- iridl:SeaSurfaceTemperatureAnomaly
- missing_value
- NaN
- pointwidth
- 1.0
- standard_name
- sea_surface_temperature
- units
- 57.2957795130823 degree_Kelvin radian-1 east
- history
- root mean sq anom $partialdiff sub X$ [ NOAA NCDC ERSST version3b anom ]
- Version 3b
Averaged over X[1W, 3W] minimum 0.0% data present
- Version 3b
References
Smith_etal2008Xue_etal2003
Last updated: Wed, 09 Mar 2022 20:30:18 GMT
Expires: Thu, 02 Apr 2020 00:00:00 GMT
Data Views
Views
data as colors
data as contours| T | Y | zlev | |
 root mean sq anom $partialdiff sub X$ [ NOAA NCDC ERSST version3b anom ] 0.0 meters[ Y zlev | T] | M | M | M |
|---|
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 Y T
- Differentiate along Y T
- Take differences along Y T
RMS (root mean square with mean *not* removed) over Y T | Y T |
RMSA (root mean square with mean removed) over Y T | Y T |
Maximum over Y T | Y T |
Minimum over Y T | Y T |
Detrend (best-fit-line) over Y T | Y T |
Note on units