data: $partialdiff sub T$ $integral dT$ [ LEVITUS SEASONAL sal ]

served from IRI/LDEO Climate Data Library

∂_T ∫dT [ LEVITUS SEASONAL sal ] : ∂_T data

SEASONAL sal int_dT ∂_T from LEVITUS: Objectively analyzed fields of major ocean parameters at the annual, seasonal, and monthly time scales; Superceded by LEVITUS94.

Independent Variables (Grids)

Time: grid: /T (months since 1960-01-01) ordered (Feb-Apr 1960) to (Nov 1960 - Jan 1961) by 3.0 N= 4 pts :grid
Longitude: grid: /X (degree_east) periodic (0.5E) to (0.5W) by 1.0 N= 360 pts :grid
Latitude: grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 1.0 N= 180 pts :grid
Depth: grid: /Z (unitless) ordered [ (0.0) (10.0) (20.0) (30.0) (50.0) (75.0) (100.0) (125.0) (150.0) (200.0) (250.0) (300.0) (400.0) (500.0) (600.0) (700.0) (800.0) (900.0) (1000.0) (1100.0) (1200.0) (1300.0) (1400.0) (1500.0)] :grid

Other Info

CE: null
CS: null
datatype: realarraytype
file_missing_value: -1.00000000E10
missing_value: NaN
units: p.s.u^. months /months
history: Levitus Climatological Temperature and Salinity -- Seasonal

References

Levitus, S. E.. Climatological atlas of the world ocean, NOAA Professional Paper 13, US Government Printing Office, Washington DC, 1982

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

Data Views

	T	X	Y	Z
$partialdiff sub T$ $integral dT$ [ LEVITUS SEASONAL sal ] [ Y Z X \| T]	M	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 Y Z X T
Differentiate along Y Z X T
Take differences along Y Z X T