data: $integral dT$ $integral dT$ [ NOAA NCDC ERSST version5 sst ]

∫dT ∫dT [ NOAA NCDC ERSST version5 sst ] : Extended reconstructed sea surface temperature data

sst sst sst int_dT Extended reconstructed sea surface temperature from NOAA NCDC ERSST version5: ERSST.v5: Extended Reconstructed Sea Surface Temperature Dataset, Version 5..

Independent Variables (Grids)

Time: grid: /T (days since 1960-01-01) ordered [ (1200 16 Dec 1853) (1200 16 Jan 1854) (0000 15 Feb 1854) ... (0000 15 Mar 2023)] N= 2032 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (1E) to (1W) 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

bufferwordsize: 8
CE: null
CS: null
datatype: doublearraytype
file_missing_value: -999.0
iridl:hasSemantics: iridl:SeaSurfaceTemperature
missing_value: NaN
pointwidth: 1.0
standard_name: sea_surface_temperature
units: 7464960000 degree_Kelvin second²udunits(3): Invalid integer udunits(3): Invalid integer
standard units*

References

Huang_etal2017

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

Data Views

	T	X	Y	zlev
NOAA NCDC ERSST version5[sst anom ]
$integral dT$ $integral dT$ [ 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