served from IRI/LDEO Climate Data Library
IGOSS TOPEX UTCSR ssh climatology: Sea Surface Height data
ssh ssh Sea Surface Height from IGOSS TOPEX UTCSR: University of Texas at Austin Center for Space Research TOPEX/POSEIDON Gridded Sea Level Anomalies.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 01-Jan) periodic (Oct) to (Sep) by 1.0 N= 12 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (0) to (1W) by 1.0 N= 360 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (74.5S) to (74.5N) by 1.0 N= 150 pts :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- file_missing_value
- 999.0
- missing_value
- NaN
- units
- cm
- standard units*
- 0.01 meter
- history
- IGOSS TOPEX UTCSR ssh
- Monthly mean sea surface height. USA
IGOSS TOPEX UTCSR ssh climatology- Averaged over T2[Oct 1992 - Sep 1993, Oct 1993 - Sep 1994] minimum 0.0% data present
References
Tapley et al., Accuracy assessment of the large-scale dynamic ocean topography from TOPEX/POSEIDON altimetry, J. Geophys. Res., 99(C12), 24605-24617,1994.
Last updated: Tue, 19 May 2015 19:17:47 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 IGOSS TOPEX UTCSR ssh climatology[ 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