data: $partialdiff sub T$ [ NOAA NCEP EMC CMB Pacific weekly swfx ]

served from IRI/LDEO Climate Data Library

∂_T [ NOAA NCEP EMC CMB Pacific weekly swfx ]: ∂_T short wave flux data

weekly swfx ∂_T short wave flux from NOAA NCEP EMC CMB Pacific: Pacific Ocean Hindcast data derived from a model-based ocean analysis system.

Independent Variables (Grids)

Time (time): grid: /T (julian_day) ordered (1200 1 Jan 1997 - 1200 8 Jan 1997) to (1200 26 Jan 2005 - 1200 2 Feb 2005) by 7.0 N= 422 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (122.25E) to (71.25W) by 1.5 N= 112 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (35S) to (45N) by 1.0 N= 81 pts :grid

Other Info

missing_value: NaN
units: 0.484259259259259 kilogram second^-4

References

Behringer, D. W., M. Ji, and A. Leetmaa, 1998: An Improved coupled model for ENSO prediction and implications for ocean initialization. Part I: The ocean data assimilation system. Mon. Wea. Rev., 126, 1013-1021.

Ji, M., A. Leetmaa, and J. Derber, 1995: An ocean analysis system for seasonal to interannual climate studies. Mon. Wea. Rev., 123, 460-481.

Ji, M., and T. M. Smith, 1995: Ocean model response to temperature data and varying surface wind stress: Intercomparisons and Implications for climate forecast. Mon. Wea. Rev., 123, 1811-1821.

Last updated: Wed, 13 Feb 2019 20:27:28 GMT

Data Views

	T	X	Y
$partialdiff sub T$ [ NOAA NCEP EMC CMB Pacific weekly swfx ][ 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