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max ∫dT max [ KAPLAN EXTENDED v2 ssta ] : SST anomaly\0~ data
ssta max 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 . isIndependent Variables (Grids)
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
- $integral dT$ max [ KAPLAN EXTENDED v2 ssta ] 0000 1 Aug 2014
- OS extended by NCEP\0$G
max over X[27.5E, 22.5E]
max $integral dT$ max [ KAPLAN EXTENDED v2 ssta ]- max over Y[87.5S, 87.5N] T[0000 1 Jan 1856, 0000 1 Aug 2014]
- OS extended by NCEP\0$G
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, 1998R. 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
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
- Differentiate along
- Take differences along
RMS (root mean square with mean *not* removed) over
RMSA (root mean square with mean removed) over
Maximum over
Minimum over
Detrend (best-fit-line) over
Note on units