data: NOAA NCDC ERSST version3b err

NOAA NCDC ERSST version3b err: Estimated error standard deviation of analyzed_ersst data

err 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 (days since 1960-01-01) ordered [ (Jan 1854) (Feb 1854) (Mar 1854) ... (Oct 2017)] N= 1966 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (0) to (2W) 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

datatype: shortarraytype
missing_value: -999
pointwidth: 1.0
scale_factor: 0.01
units: degree_Celsius
valid_max: 1000
valid_min: 0
standard units*: degree_Kelvin
history: Version 3b

References

Smith_etal2008

Xue_etal2003

Last updated: Wed, 20 Mar 2019 09:34:10 GMT
Expires: Tue, 02 Oct 2018 00:00:00 GMT

Data Views

	T	X	Y	zlev
NOAA NCDC ERSST version3b[sst err anom ]
grid: /X (degree_east) periodic (0) to (2W) by 2.0 N= 180 pts :grid		M
grid: /Y (degree_north) ordered (88S) to (88N) by 2.0 N= 89 pts :grid			M
grid: /T (days since 1960-01-01) ordered [ (Jan 1854) (Feb 1854) (Mar 1854) ... (Oct 2017)] N= 1966 pts :grid	M
NOAA NCDC ERSST version3b err 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