data: max root mean sq [ NOAA NCDC ERSST version3b sst climatology ]

max root mean sq [ NOAA NCDC ERSST version3b sst climatology ] : Extended reconstructed sea surface temperature data

sst sst sst Extended reconstructed sea surface temperature from NOAA NCDC ERSST version3b: ERSST.v3b: Extended Reconstructed Sea Surface Temperature Dataset, Verson 3b.

Independent Variables (Grids)

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

bufferwordsize

CE

null

CS

null

datatype

doublearraytype

iridl:hasSemantics

iridl:SeaSurfaceTemperature

missing_value

NaN

pointwidth

1.0

units

degree_Celsius

standard units*

degree_Kelvin

history

NOAA NCDC ERSST version3b sst climatology

Version 3b
Averaged over T2[1854, 2014] minimum 0.0% data present

root mean sq [ NOAA NCDC ERSST version3b sst climatology ]

Averaged over T[Jan, Dec] minimum 0.0% data present

max root mean sq [ NOAA NCDC ERSST version3b sst climatology ]

max over X[0, 2W]

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: Thu, 11 Jun 2015 13:35:46 GMT
Expires: Thu, 02 Jul 2015 00:00:00 GMT

Data Views

	Y	zlev
max root mean sq [ NOAA NCDC ERSST version3b sst climatology ] 0.0 meters[ Y 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 Y
Differentiate along Y
Take differences along Y