data: $integral dX$ [ NOAA NCDC ERSST version5 sst ] anomalies

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

sst sst sst sst int_dX 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) (360) ordered [ (2354 30 Oct 1852 - 2354 1 Nov 1852) (2354 3 Apr 1853 - 2354 4 Apr 1853) (2354 5 Nov 1853 - 2354 6 Nov 1853) ... (0002 15 Sep 2023 - 0002 16 Sep 2023)] N= 379 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

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: 0.0174532925199433 degree_Kelvin radian east
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
$integral dX$ [ NOAA NCDC ERSST version5 sst ] 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