data: mean $partialdiff sub X$ $integral dT$ detrended-bfl [ NOAA NCDC ERSST version3b sst ]

mean ∂_X ∫dT detrended-bfl [ NOAA NCDC ERSST version3b sst ] : ∂_X Extended reconstructed sea surface temperature data

sst adif int_dT partial_X ∂_X Extended reconstructed sea surface temperature from NOAA NCDC ERSST version3b: ERSST.v3b: Extended Reconstructed Sea Surface Temperature Dataset, Verson 3b.

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (0000 1 Jan 1854) to (0000 1 Jan 2026) by 1.0 N= 2065 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

bufferwordsize

CE

null

CS

null

datatype

doublearraytype

iridl:hasSemantics

iridl:SeaSurfaceTemperature

missing_value

NaN

pointwidth

1.0

units

4.77464829275686 degree_Kelvin radian^-1 east year

history

mean $partialdiff sub X$ $integral dT$ detrended-bfl [ NOAA NCDC ERSST version3b sst ]

Version 3b
Averaged over X[2W, 2W] Y[89S, 89N] minimum 0.0% data present

References

Redland error: BDB V4.1+ open of '/ingrid-tmp/referencelist-sp2o.db' failed - No such file or directory

Last updated: Tue, 13 Aug 2024 08:17:43 GMT
Expires: Mon, 02 Sep 2024 00:00:00 GMT

Data Views

	T	zlev
mean $partialdiff sub X$ $integral dT$ detrended-bfl [ NOAA NCDC ERSST version3b sst ] 0.0 meters[ zlev \| T]	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 T
Differentiate along T
Take differences along T