data: max [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology sst ]

max [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology sst ]: Sea Surface Temperature data

pentad-climatology sst Sea Surface Temperature from NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2: SST fields updated from version 1 with more COADS data, new sea-ice to SST conversion algorithm, and 1971-2000 climatology.

Independent Variables (Grids)

Time: grid: /T (pentads since 1960-01-01) periodic (1-5 Jan) to (27-31 Dec) by 1.0 N= 73 pts :grid

Other Info

CE

colorscalename

sstcolorscale

CS

-2

datatype

realarraytype

file_missing_value

-999.90002

missing_value

NaN

scale_max

35.0

scale_min

-2.0

units

Celsius_scale

standard units*

degree_Kelvin above 273.15

history

max [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology sst ]

Averaged over T[Jan, Dec] minimum 0.0% data present
max over X[0.5E, 0.5W] Y[89.5S, 89.5N]

colorscale

References

Reynolds, R.W., N.A. Rayner, T.M. Smith, D.C. Stokes, and W. Wang, 2002: An Improved In Situ and Satellite SST Analysis for Climate. J. Climate, 15, 1609-1625.

Last updated: Tue, 09 Jan 2018 17:35:48 GMT

Data Views

	T
NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology[sst ]
max [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology sst ][ \| T]	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 T
Differentiate along T
Take differences along T