data: detrended-bfl $integral dT$ [ NOAA NCDC ERSST version3b anom ]

detrended-bfl ∫dT [ NOAA NCDC ERSST version3b anom ] : Extended reconstructed SST anomalies data

anom anom int_dT int_dT Extended reconstructed SST anomalies from NOAA NCDC ERSST version3b: ERSST.v3b: Extended Reconstructed Sea Surface Temperature Dataset, Verson 3b.

Independent Variables (Grids)

Time: grid: /T (days since 1960-01-01) ordered [ (1200 16 Dec 1853 - 1200 16 Jan 1854) (1200 16 Jan 1854 - 2400 14 Feb 1854) (0000 15 Feb 1854 - 1200 16 Mar 1854) ... (1200 15 Feb 2020 - 1200 15 Mar 2020)] N= 1995 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (1E) to (1W) by 2.0 N= 180 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:SeaSurfaceTemperatureAnomaly
missing_value: NaN
pointwidth: 1.0
standard_name: sea_surface_temperature
units: 86400 degree_Kelvin second
history: Version 3b

References

Smith_etal2008

Xue_etal2003

Last updated: Wed, 09 Mar 2022 20:30:18 GMT
Expires: Thu, 02 Apr 2020 00:00:00 GMT

Data Views

	T	X	Y	zlev
NOAA NCDC ERSST version3b[sst anom IOD ]
detrended-bfl $integral dT$ [ NOAA NCDC ERSST version3b anom ] 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