served from IRI/LDEO Climate Data Library
∫dT ∫dT [ FSU SMOOTH4yr ANOM tauy ] : meridional wind stress data
tauy int_dT meridional wind stress from FSU SMOOTH4yr ANOM: Spatial and temporal smoothing of FSU 4yr ANOM.Independent Variables (Grids)
- D
- grid: /D (character) unordered [ (tauy)] :grid
- Time (time)
- grid: /T (months since 1960-01-01) ordered (0000 16 Dec 1963) to (0000 16 Mar 2002) by 1.0 N= 460 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (124E) to (70W) by 2.0 N= 84 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (29S) to (29N) by 2.0 N= 30 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- units
- 0.000694444444444444 kilogram meter-1 second-2 year2
References
Legler, D.M., and J.J. O'Brien, 1988; Tropical Pacific wind stress analysis for TOGA, IOC Time series of ocean measurements, IOC Technical Series 33, Volume 4, UNESCO.
Last updated: Mon, 12 Sep 2016 21:27:17 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| D | T | X | Y | |
 $integral dT$ $integral dT$ [ FSU SMOOTH4yr ANOM tauy ] tauy[ X Y D | 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 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