data: max [ NOAA NCDC ERSST version3b anom ]

max [ NOAA NCDC ERSST version3b anom ]: Extended reconstructed SST anomalies data

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

Independent Variables (Grids)

Longitude (longitude): grid: /X (degree_east) periodic (0) to (2W) by 2.0 N= 180 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

datatype

realarraytype

file_missing_value

-999.0

iridl:hasSemantics

iridl:SeaSurfaceTemperatureAnomaly

missing_value

NaN

pointwidth

1.0

standard_name

sea_surface_temperature

units

degree_Celsius

valid_max

12.0

valid_min

-12.0

standard units*

degree_Kelvin

history

max [ NOAA NCDC ERSST version3b anom ]

Version 3b
max over Y[88S, 88N] T[Jan 1854, Feb 2020]

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

Data Views

	X	zlev
NOAA NCDC ERSST version3b[IOD anom sst ]
max [ NOAA NCDC ERSST version3b anom ] 0.0 meters[ X 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 X
Differentiate along X
Take differences along X