data: min $partialdiff sub T$ $integral dY$ [ NOAA NCDC ERSST version3b anom ]

min ∂_T ∫dY [ NOAA NCDC ERSST version3b anom ] : ∂_T Extended reconstructed SST anomalies data

anom anom int_dY partial_T ∂_T 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 (16 Jan 1854 - 15 Feb 1854) to (16 Jan 2020 - 15 Feb 2020) by 1.0 N= 1993 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

realarraytype

file_missing_value

-999.0

iridl:hasSemantics

iridl:SeaSurfaceTemperatureAnomaly

missing_value

NaN

pointwidth

1.0

standard_name

sea_surface_temperature

units

0.20943951023932 degree_Kelvin radian north year^-1

history

min $partialdiff sub T$ $integral dY$ [ NOAA NCDC ERSST version3b anom ]

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

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	Y	zlev
NOAA NCDC ERSST version3b[sst IOD anom ]
min $partialdiff sub T$ $integral dY$ [ 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