served from IRI/LDEO Climate Data Library
WEARE MONTHLY taux climatology: zonal wind stress data
MONTHLY taux zonal wind stress from WEARE: Marine climate atlas of the tropical Pacific Ocean.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 01-Jan) periodic (Jan) to (Dec) by 1.0 N= 12 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (112.5E) to (72.5W) by 5.0 N= 36 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (37.5S) to (27.5N) by 5.0 N= 14 pts :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- file_missing_value
- 1.00000002E30
- missing_value
- NaN
- units
- dyne /cm2
- standard units*
- 0.1 kilogram meter-1 second-2
- history
- WEARE MONTHLY taux climatology
- Weare averaged surface data
Averaged over T2[1957, 1976] minimum 0.0% data present
- Weare averaged surface data
References
Weare, B. C., P. T. Strub, M. D. Samuel. Marine climate atlas of the tropical Pacific Ocean, number 20, 1980Weare, B. C., P. T. Strub, M. D. Samuel. Annual mean surface heat fluxes in the tropical Pacific Ocean. J. Phys. Oceanogr. 11, 1981
Last updated: Mon, 12 Sep 2016 21:13:53 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts
line plots
color bars| T | X | Y | |
 WEARE MONTHLY taux climatology[ Y X 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 Y X T
- Differentiate along Y X T
- Take differences along Y X T
RMS (root mean square with mean *not* removed) over Y X T | Y X Y T X T | Y X T |
RMSA (root mean square with mean removed) over Y X T | Y X Y T X T | Y X T |
Maximum over Y X T | Y X Y T X T | Y X T |
Minimum over Y X T | Y X Y T X T | Y X T |
Detrend (best-fit-line) over Y X T | Y X Y T X T | Y X T |
Note on units