served from IRI/LDEO Climate Data Library
∂Y ∫dT ∫dX ∫dT ∂T detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ] anomalies anomalies: ∂Y ∂T Sea Surface Height Anomaly data
ssha adif adif partial_T int_dT int_dT int_dX int_dX int_dT partial_Y partial_Y ∂Y ∂T 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 1 Oct 1992) to (0000 1 Aug 2002) by 1.0 N= 119 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (0) to (0) by 4.0 N= 91 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (58.5S) to (58.5N) by 1.0 N= 118 pts :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- missing_value
- NaN
- units
- 0.000833333333333335 meter year
- history
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ] anomalies
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- Monthly mean sea surface height anomaly. USA
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ] climatology
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- Monthly mean sea surface height anomaly. USA
Averaged over T2[16 Sep 1992 - 15 Sep 1993, 16 Sep 2000 - 15 Sep 2001] minimum 0.0% data present
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ] anomalies climatology
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- Monthly mean sea surface height anomaly. USA
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ] climatology
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- Monthly mean sea surface height anomaly. USA
Averaged over T2[16 Sep 1992 - 15 Sep 1993, 16 Sep 2000 - 15 Sep 2001] minimum 0.0% data present
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ]
- $partialdiff sub Y$ $integral dT$ $integral dX$ $integral dT$ $partialdiff sub T$ detrended-bfl detrended-bfl [ IGOSS TOPEX NOAA ssha ] anomalies
References
page 0: illegal page type or format PANIC: Invalid argument PANIC: fatal region error detected; run recovery PANIC: fatal region error detected; run recovery Cheney_etal1994Last updated: Wed, 13 Feb 2019 20:27:28 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