served from IRI/LDEO Climate Data Library
∫dX [ NOAA NCEP EMC CMB Pacific weekly swfx ]: short wave flux data
weekly swfx 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 (29 Dec 1996 - 4 Jan 1997) to (30 Jan 2005 - 5 Feb 2005) by 7.0 N= 423 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (121.5E) to (70.5W) by 1.5 N= 113 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (35S) to (45N) by 1.0 N= 81 pts :grid
Other Info
- bufferwordsize
- 8
- datatype
- doublearraytype
- missing_value
- NaN
- units
- 730.245759034427 kilogram radian east second-3
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_etal1995
Ji_Smith1995
Last updated: Wed, 13 Feb 2019 20:27:28 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 $integral dX$ [ 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
RMS (root mean square with mean *not* removed) over X Y T | X Y X T Y T | X Y T |
RMSA (root mean square with mean removed) over X Y T | X Y X T Y T | X Y T |
Maximum over X Y T | X Y X T Y T | X Y T |
Minimum over X Y T | X Y X T Y T | X Y T |
Detrend (best-fit-line) over X Y T | X Y X T Y T | X Y T |
Note on units