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

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

sst adif 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)

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

CE

null

CS

null

datatype

doublearraytype

iridl:hasSemantics

iridl:SeaSurfaceTemperature

missing_value

NaN

pointwidth

1.0

units

57.2957795130823 degree_Kelvin radian^-1 east

history

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

Version 3b
Averaged over X[2W, 2W] T[Jan 1854, Nov 2025] minimum 0.0% data present

References

page 0: illegal page type or format PANIC: Invalid argument PANIC: fatal region error detected; run recovery PANIC: fatal region error detected; run recovery PANIC: fatal region error detected; run recovery Smith_etal2008

Xue_etal2003

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

Data Views

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