served from IRI/LDEO Climate Data Library
detrended-bfl detrended-bfl ∫dX ∂T ∂X ∂T detrended-bfl detrended-bfl detrended-bfl detrended-bfl detrended-bfl ∫dY detrended-bfl detrended-bfl detrended-bfl [ detrended-bfl ( IGOSS TOPEX UTCSR ssh ) anomalies ] : ∂T ∂X ∂T Sea Surface Height data
ssh adif adif adif adif adif adif int_dY adif adif adif adif adif partial_T partial_X partial_T int_dX adif ∂T ∂X ∂T 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 1960-01-01) ordered (16 Nov 1992 - 15 Dec 1992) to (16 Dec 1994 - 15 Jan 1995) by 1.0 N= 26 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (1W) to (1W) by 1.0 N= 361 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (75.5S) to (75.5N) by 1.0 N= 152 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- 999.0
- missing_value
- NaN
- units
- 0.0251327412287183 meter radian east year-2
- history
- detrended-bfl [ IGOSS TOPEX UTCSR ssh ]
- Monthly mean sea surface height. USA
- detrended-bfl [ IGOSS TOPEX UTCSR ssh ] climatology
- detrended-bfl [ IGOSS TOPEX UTCSR ssh ]
- Monthly mean sea surface height. USA
Averaged over T2[Oct 1992 - Sep 1993, Oct 1993 - Sep 1994] minimum 0.0% data present
- detrended-bfl [ IGOSS TOPEX UTCSR ssh ]
- detrended-bfl [ IGOSS TOPEX UTCSR ssh ]
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
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