data: max $partialdiff sub Y$ [ NOAA NCDC ERSST version3b anom ]

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

anom partial_Y ∂_Y Extended reconstructed SST anomalies 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
Latitude (latitude): grid: /Y (degree_north) ordered (87S) to (87N) by 2.0 N= 88 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

datatype

realarraytype

iridl:hasSemantics

iridl:SeaSurfaceTemperatureAnomaly

missing_value

NaN

pointwidth

1.0

units

57.2957795130823 degree_Kelvin radian^-1 north

history

max $partialdiff sub Y$ [ NOAA NCDC ERSST version3b anom ]

Version 3b
max over X[0, 2W]

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	Y	zlev
grid: /Y (degree_north) ordered (87S) to (87N) by 2.0 N= 88 pts :grid		M
grid: /T (months since 1960-01-01) ordered (Jan 1854) to (Oct 2017) by 1.0 N= 1966 pts :grid	M
max $partialdiff sub Y$ [ NOAA NCDC ERSST version3b anom ] 0.0 meters[ Y zlev \| T]	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 Y T
Differentiate along Y T
Take differences along Y T

Average over Y T | Y T |
RMS (root mean square with mean *not* removed) over Y T | Y T |
RMSA (root mean square with mean removed) over Y T | Y T |
Maximum over Y T | Y T |
Minimum over Y T | Y T |
Detrend (best-fit-line) over Y T | Y T |

Note on units