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

served from IRI/LDEO Climate Data Library

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

ssha ssha adif int_dX int_dX partial_T int_dX int_dX int_dX partial_T adif partial_Y partial_T partial_T partial_Y adif partial_Y ∂_T ∂_Y ∂_Y ∂_T ∂_Y ∂_T ∂_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 (Jan 1993) to (Apr 2002) by 1.0 N= 112 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 (58S) to (58N) by 1.0 N= 117 pts :grid

Other Info

CE

null

CS

null

datatype

realarraytype

missing_value

NaN

units

11880.8528398328 meter radian^-1 north year^-4

history

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

Monthly mean sea surface height anomaly. USA

References

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Last updated: Wed, 13 Feb 2019 20:27:28 GMT

Data Views

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