data: $integral dT$ [ NOAA NCEP EMC CMB Pacific weekly temp ]

served from IRI/LDEO Climate Data Library

∫dT [ NOAA NCEP EMC CMB Pacific weekly temp ]: temperature data

weekly temp int_dT temperature from NOAA NCEP EMC CMB Pacific: Pacific Ocean Hindcast data derived from a model-based ocean analysis system.

Independent Variables (Grids)

Time: grid: /T (julian_day) ordered (0000 29 Dec 1996) to (0000 2 Nov 2008) by 7.0 N= 619 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (123E) to (72W) by 1.5 N= 111 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (35S) to (45N) by 1.0 N= 81 pts :grid
Depth: grid: /Z (m) ordered [ (5.0) (15.0) (25.0) (35.0) (45.0) (55.0) (65.0) (75.0) (85.0) (95.0) (106.25) (120.0) (136.25) (155.0) (177.5) (205.0) (240.0) (285.0) (345.0) (430.0) (550.0) (720.0) (967.5) (1327.5) (1821.0) (2443.5) (3126.5)] :grid

Other Info

CE: null
colorscalename: sstcolorscale
CS: null
datatype: realarraytype
missing_value: NaN
units: 86400 degree_Kelvin second
history: T: 6-12 Feb 2005 to 26 Oct 2008 - 1 Nov 2008 appended from NOAA NCEP EMC CMB Pacific godas temp

References

Behringer_etal1998

Ji_etal1995

Ji_Smith1995

Last updated: Mon, 12 Sep 2016 21:28:51 GMT

Data Views

	T	X	Y	Z
$integral dT$ [ NOAA NCEP EMC CMB Pacific weekly temp ][ X Z \| Y T]	M	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 Z Y T
Differentiate along X Z Y T
Take differences along X Z Y T