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root mean sq ∫dT detrended-bfl [ KAPLAN EXTENDED v2 ssta ] : SST anomaly\0~ data

ssta adif int_dT int_dT SST anomaly\0~ from KAPLAN EXTENDED v2: Statistically homogenous concatenation of Kaplan et al [1998] OS SST and Reynolds and Smith [1994] NCEP OI analyses; the latter gets degraded to the resolution of the former\0 àÝX ­.

Independent Variables (Grids)

Time
grid: /T (days since 1960-01-01) ordered [ (0000 1 Jan 1856) (0000 1 Feb 1856) (0000 1 Mar 1856) ... (0000 1 Aug 2014)] N= 1904 pts :grid
Longitude
grid: /X (degree_east) periodic (27.5E) to (22.5E) by 5.0 N= 72 pts :grid

Other Info

bufferwordsize
8
CE
null
CS
null
datatype
doublearraytype
file_missing_value
1.00000002E30
missing_value
NaN
units
0.0833333333333333 degree_Kelvin year
history
root mean sq $integral dT$ detrended-bfl [ KAPLAN EXTENDED v2 ssta ]
OS extended by NCEP\0$G 
Averaged over Y[90S, 90N] minimum 0.0% data present

References

Kaplan, A., M. Cane, Y. Kushnir, A. Clement, M. Blumenthal, and B. Rajagopalan, Analyses of global sea surface temperature 1856-1991, Journal of Geophysical Research, 103, 18,567-18,589, 1998

R. W. Reynolds, T. M. Smith. Improved global sea surface temperature analyses.. J. Climate 7, 1994

Last updated: Tue, 29 Mar 2016 08:02:46 GMT

Data Views

TX
[ X | T]MM


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. Average over X T | X T |
RMS (root mean square with mean *not* removed) over X T | X T |
RMSA (root mean square with mean removed) over X T | X T |
Maximum over X T | X T |
Minimum over X T | X T |
Detrend (best-fit-line) over X T | X T |
Convert units from 0.0833333333333333 degree_Kelvin year to

Note on units