data: detrended-bfl $partialdiff sub T$ $integral dT$ $integral dT$ $integral dT$ $partialdiff sub X$ detrended-bfl $integral dT$ detrended-bfl $integral dX$ detrended-bfl $partialdiff sub X$ $integral dX$ detrended-bfl [ IGOSS TOPEX NOAA ssha ]

served from IRI/LDEO Climate Data Library

detrended-bfl ∂_T ∫dT ∫dT ∫dT ∂_X detrended-bfl ∫dT detrended-bfl ∫dX detrended-bfl ∂_X ∫dX detrended-bfl [ IGOSS TOPEX NOAA ssha ] : ∂_T ∂_X ∂_X Sea Surface Height Anomaly data

ssha ssha adif int_dX partial_X adif int_dX adif int_dT adif partial_X int_dT int_dT int_dT partial_T ∂_T ∂_X ∂_X 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 (Sep 1992) to (Aug 2002) by 1.0 N= 120 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (2E) to (2W) by 4.0 N= 90 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (60S) to (60N) by 1.0 N= 121 pts :grid

Other Info

bufferwordsize

CE

null

CS

null

datatype

doublearraytype

missing_value

NaN

units

5.78703703703705×10^-06 meter year³

history

detrended-bfl $partialdiff sub T$ $integral dT$ $integral dT$ $integral dT$ $partialdiff sub X$ detrended-bfl $integral dT$ detrended-bfl $integral dX$ detrended-bfl $partialdiff sub X$ $integral dX$ detrended-bfl [ IGOSS TOPEX NOAA ssha ]

Monthly mean sea surface height anomaly. USA

References

Cheney_etal1994

Last updated: Fri, 18 Sep 2015 18:39:07 GMT

Data Views

	T	X	Y
detrended-bfl $partialdiff sub T$ $integral dT$ $integral dT$ $integral dT$ $partialdiff sub X$ detrended-bfl $integral dT$ detrended-bfl $integral dX$ detrended-bfl $partialdiff sub X$ $integral dX$ detrended-bfl [ IGOSS TOPEX NOAA ssha ] [ 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