served from IRI/LDEO Climate Data Library
∫dY ∫dY ∫dT ∫dT [ IGOSS TOPEX NOAA ssha ] : Sea Surface Height Anomaly data
ssha ssha int_dT int_dT int_dY Sea Surface Height Anomaly from IGOSS TOPEX NOAA: NOAA TOPEX/POSEIDON Altimeter Gridded Sea Level Analysis.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 1960-01-01) ordered (0000 16 Sep 1992) to (0000 16 Aug 2002) by 1.0 N= 120 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (2E) to (2W) by 4.0 N= 90 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (60.5S) to (60.5N) by 1.0 N= 122 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- missing_value
- NaN
- units
- 2.11539874851881×10-08 meter radian2 north year2
- history
- $integral dY$ $integral dY$ $integral dT$ $integral dT$ [ IGOSS TOPEX NOAA ssha ]
- Monthly mean sea surface height anomaly. USA
References
Cheney, B., L. Miller, R. Agreen, N. Doyle, and J. Lillibridge. 1994. TOPEX/POSEIDON: The 2-cm Solution. J. Geophys. Res., 99 (C12), 24555-24564.
Last updated: Fri, 18 Sep 2015 18:39:07 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts
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