data: max $integral dY$ $partialdiff sub X$ [ NOAA NCDC ERSST version3b err anomalies ]

max ∫dY ∂_X [ NOAA NCDC ERSST version3b err anomalies ] : ∂_X Estimated error standard deviation of analyzed_ersst data

err err partial_X int_dY ∂_X Estimated error standard deviation of analyzed_ersst 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 (Jan 1854) to (Nov 2025) by 1.0 N= 2063 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

bufferwordsize

CE

null

CS

null

datatype

doublearraytype

missing_value

NaN

pointwidth

1.0

units

degree_Celsius

standard units*

degree_Kelvin

history

NOAA NCDC ERSST version3b err
Version 3b

NOAA NCDC ERSST version3b err climatology

Version 3b
Averaged over T2[1854, 2024] minimum 0.0% data present

max $integral dY$ $partialdiff sub X$ [ NOAA NCDC ERSST version3b err anomalies ]

max over X[1W, 3W] Y[89S, 89N]

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

	T	zlev
max $integral dY$ $partialdiff sub X$ [ NOAA NCDC ERSST version3b err anomalies ] 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