data: $integral dX$ [ NOAA NCDC ERSST version3b anom ]

∫dX [ NOAA NCDC ERSST version3b anom ]: Extended reconstructed SST anomalies data

anom int_dX int_dX 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 (days since 1960-01-01) ordered [ (16 Jan 1854 - 15 Feb 1854) (16 Feb 1854 - 15 Mar 1854) (16 Mar 1854 - 15 Apr 1854) ... (16 Sep 2017 - 15 Oct 2017)] N= 1965 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (1W) to (1W) by 2.0 N= 181 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

datatype: realarraytype
iridl:hasSemantics: iridl:SeaSurfaceTemperatureAnomaly
missing_value: NaN
pointwidth: 1.0
units: 0.0174532925199433 degree_Kelvin radian east
history: Version 3b

References

Smith_etal2008

Xue_etal2003

Last updated: Wed, 20 Mar 2019 09:34:10 GMT
Expires: Tue, 02 Oct 2018 00:00:00 GMT

Data Views

	T	X	Y	zlev
$integral dX$ [ NOAA NCDC ERSST version3b anom ] 0.0 meters[ X Y zlev \| T]	M	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 X Y T
Differentiate along X Y T
Take differences along X Y T