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

served from IRI/LDEO Climate Data Library

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

ssha adif adif adif adif partial_X partial_X adif partial_T partial_Y partial_Y int_dT ∂_Y ∂_Y ∂_T ∂_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 (Oct 1992) to (Jul 2002) by 1.0 N= 118 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 (58.5S) to (58.5N) by 1.0 N= 118 pts :grid

Other Info

bufferwordsize

CE

null

CS

null

datatype

doublearraytype

missing_value

NaN

units

1880.90948814419 meter radian^-3 east

history

detrended-bfl $integral dT$ $partialdiff sub Y$ $partialdiff sub Y$ $partialdiff sub T$ detrended-bfl $partialdiff sub X$ detrended-bfl detrended-bfl detrended-bfl [ 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: Tue, 19 May 2015 19:52:55 GMT

Data Views

	T	X	Y
detrended-bfl $integral dT$ $partialdiff sub Y$ $partialdiff sub Y$ $partialdiff sub T$ detrended-bfl $partialdiff sub X$ detrended-bfl detrended-bfl 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