data: root mean sq detrended-bfl [ NOAA NCDC ERSST version3b sst ]

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

sst adif 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 (Jan 1854) to (Oct 2017) by 1.0 N= 1966 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

bufferwordsize

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

degree_Celsius

standard units*

degree_Kelvin

history

root mean sq detrended-bfl [ NOAA NCDC ERSST version3b sst ]

Version 3b
Averaged over X[1W, 1W] Y[89S, 89N] minimum 0.0% data present

References

Smith, T.M., R.W. Reynolds, Thomas C. Peterson, and Jay Lawrimore, 2008: Improvements to NOAA's Historical Merged Land-Ocean Surface Temperature Analysis (1880-2006). Journal of Climate, 21, 2283-2296.

Xue, Y., T. M. Smith, and R. W. Reynolds, 2003: Interdecadal changes of 30-yr SST normals during 1871-2000. J. Climate, 16, 1601-1612.

Last updated: Wed, 01 Feb 2023 14:07:40 GMT
Expires: Thu, 02 Feb 2023 00:00:00 GMT

Data Views

	T	zlev
root mean sq 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