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

served from IRI/LDEO Climate Data Library

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

ssha adif adif partial_T int_dT adif partial_X adif partial_T partial_T partial_T adif int_dX adif adif adif ∂_T ∂_X ∂_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 (Nov 1992) to (Jun 2002) by 1.0 N= 116 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (2E) to (6W) by 4.0 N= 89 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (59.5S) to (59.5N) by 1.0 N= 120 pts :grid

Other Info

bufferwordsize

CE

null

CS

null

datatype

doublearraytype

missing_value

NaN

units

0.12 meter year^-1

history

detrended-bfl detrended-bfl $integral dX$ detrended-bfl $partialdiff sub T$ detrended-bfl $partialdiff sub X$ detrended-bfl $integral dT$ $partialdiff sub T$ 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: Wed, 13 Feb 2019 20:27:28 GMT

Data Views

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