data: max [ NOAA NCDC ERSST version5 sst climatology ]

max [ NOAA NCDC ERSST version5 sst climatology ]: Extended reconstructed sea surface temperature data

sst sst max Extended reconstructed sea surface temperature from NOAA NCDC ERSST version5: ERSST.v5: Extended Reconstructed Sea Surface Temperature Dataset, Version 5..

Independent Variables (Grids)

Time (time): grid: /T (days since 1960-01-01) ordered [ (Jan 1960) (Feb 1960) (Mar 1960) (Apr 1960) (May 1960) (Jun 1960) (Jul 1960) (Aug 1960) (Sep 1960) (Oct 1960) (Nov 1960) (Dec 1960)] :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

CE

null

CS

null

datatype

realarraytype

file_missing_value

-999.0

iridl:hasSemantics

iridl:SeaSurfaceTemperature

missing_value

NaN

pointwidth

1.0

standard_name

sea_surface_temperature

units

Celsius_scale

standard units*

degree_Kelvin above 273.15

history

max [ NOAA NCDC ERSST version5 sst climatology ]

Averaged over T2[1854, 2018] minimum 0.0% data present
max over X[0, 2W]

References

Huang_etal2017

Last updated: Wed, 05 Feb 2020 11:55:24 GMT
Expires: Tue, 02 Apr 2019 00:00:00 GMT

Data Views

	T	Y	zlev
max [ NOAA NCDC ERSST version5 sst climatology ] 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