data: $partialdiff sub T$ [ $partialdiff sub T$ ( NOAA NCDC ERSST version5 anom ) anomalies ]

∂_T [ ∂_T ( NOAA NCDC ERSST version5 anom ) anomalies ]: ∂_T ∂_T Extended reconstructed SST anomalies data

anom anom anom partial_T partial_T partial_T ∂_T ∂_T Extended reconstructed SST anomalies 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) (360) ordered [ (1154 30 Aug 1852 - 1154 1 Nov 1852) (1154 1 Nov 1852 - 1154 2 Jan 1853) (1154 2 Jan 1853 - 1154 3 Feb 1853) ... (1202 16 Nov 2023 - 1202 17 Dec 2023)] N= 1223 pts :grid
longitude (longitude): grid: /X (degree_east) periodic (0) to (2W) by 2.0 N= 180 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (87S) to (87N) by 2.0 N= 88 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

CE: null
colorscalename: sstacolorscale
CS: null
datatype: realarraytype
file_missing_value: -999.0
iridl:hasSemantics: iridl:SeaSurfaceTemperatureAnomaly
maxncolor: 254
missing_value: NaN
pointwidth: 1.0
standard_name: sea_surface_temperature
units: 0.000138888888888889 degree_Kelvin second^-1 year^-1
history: Averaged over T2[Feb 1854 - Jan 1855, Feb 2022 - Jan 2023] minimum 0.0% data present

References

Huang_etal2017

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

Data Views

	T	X	Y	zlev
$partialdiff sub T$ [ $partialdiff sub T$ ( NOAA NCDC ERSST version5 anom ) anomalies ] 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