data: KAPLAN EXTENDED v2 ssta

KAPLAN EXTENDED v2 ssta: SST anomaly data

ssta SST anomaly 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.

Independent Variables (Grids)

Time: grid: /T (days since 1960-01-01) ordered [ (Jan 1856) (Feb 1856) (Mar 1856) ... (Nov 2013)] N= 1895 pts :grid
Longitude: grid: /X (degree_east) periodic (27.5E) to (22.5E) by 5.0 N= 72 pts :grid
Latitude: grid: /Y (degree_north) ordered (87.5S) to (87.5N) by 5.0 N= 36 pts :grid

Other Info

datatype: realarraytype
missing_value: 1.00000002E30
units: degree_Celsius
standard units*: degree_Kelvin
history: OS extended by NCEP

References

page 0: illegal page type or format PANIC: Invalid argument PANIC: fatal region error detected; run recovery PANIC: fatal region error detected; run recovery PANIC: fatal region error detected; run recovery Kaplan_etal1998

Reynolds_Smith1994

Last updated: Wed, 09 Mar 2022 20:30:18 GMT

Data Views

	T	X	Y
grid: /X (degree_east) periodic (27.5E) to (22.5E) by 5.0 N= 72 pts :grid		M
grid: /Y (degree_north) ordered (87.5S) to (87.5N) by 5.0 N= 36 pts :grid			M
grid: /T (days since 1960-01-01) ordered [ (Jan 1856) (Feb 1856) (Mar 1856) ... (Nov 2013)] N= 1895 pts :grid	M
KAPLAN EXTENDED v2 ssta[ X Y \| 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 X Y T
Differentiate along X Y T
Take differences along X Y T