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

served from IRI/LDEO Climate Data Library

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

ssha adif adif int_dT int_dT adif adif adif adif partial_Y partial_Y partial_Y partial_Y partial_Y int_dY adif int_dT ∂_Y ∂_Y ∂_Y 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 Sep 1992) to (0000 1 Sep 2002) by 1.0 N= 121 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (6E) to (2E) by 4.0 N= 90 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (58S) to (58N) by 1.0 N= 117 pts :grid

Other Info

CE

null

CS

null

datatype

realarraytype

missing_value

NaN

units

0.0189977219329383 meter radian^-2 north year³

history

$partialdiff sub Y$ $integral dT$ detrended-bfl $integral dY$ $partialdiff sub Y$ $partialdiff sub Y$ detrended-bfl detrended-bfl detrended-bfl detrended-bfl $integral dT$ $integral dT$ 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
$partialdiff sub Y$ $integral dT$ detrended-bfl $integral dY$ $partialdiff sub Y$ $partialdiff sub Y$ detrended-bfl detrended-bfl detrended-bfl detrended-bfl $integral dT$ $integral dT$ 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