data: $partialdiff sub X$ $partialdiff sub T$ [ NOAA NCDC ERSST version5 sst ]

∂_X ∂_T [ NOAA NCDC ERSST version5 sst ] : ∂_X ∂_T Extended reconstructed sea surface temperature data

sst sst sst partial_T partial_X ∂_X ∂_T Extended reconstructed sea surface temperature from NOAA NCDC ERSST version5: ERSST.v5: Extended Reconstructed Sea Surface Temperature Dataset, Version 5..

Independent Variables (Grids)

Time (time): grid: /T (days since 1960-01-01) ordered [ (0000 15 Feb 1854 - 1800 16 Mar 1854) (1800 16 Mar 1854 - 2400 15 Apr 1854) (0000 16 Apr 1854 - 1200 16 May 1854) ... (1500 16 Dec 2022 - 0300 16 Jan 2023)] N= 2027 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (1W) to (3W) by 2.0 N= 180 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
file_missing_value: -999.0
iridl:hasSemantics: iridl:SeaSurfaceTemperature
missing_value: NaN
pointwidth: 1.0
standard_name: sea_surface_temperature
units: 0.000663145596216232 degree_Kelvin radian^-1 east second^-1

References

Redland error: BDB V4.1+ open of '/ingrid-tmp/referencelist-so2p.db' failed - Permission denied

Last updated: Mon, 27 Mar 2023 13:29:42 GMT

Data Views

	T	X	Y	zlev
$partialdiff sub X$ $partialdiff sub T$ [ NOAA NCDC ERSST version5 sst ] 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