data: $integral dT$ detrended-bfl [ $integral dT$ ( OLE2 ROMS-BACKUP salt ) climatology ]

served from 129.236.110.25

∫dT detrended-bfl [ ∫dT ( OLE2 ROMS-BACKUP salt ) climatology ] : Salinidad data

∫dT detrended-bfl [ ∫dT ( OLE2 ROMS-BACKUP salt ) climatology ] .

Independent Variables (Grids)

eta_rho: grid: /eta_rho (unitless) ordered (NaN) to (NaN) by NaN N= 324 pts :grid
s_rho: grid: /s_rho (unitless) ordered (NaN) to (NaN) by NaN N= 32 pts :grid
Time (time): grid: /T (days since 1960-01-01) ordered [ (1200 16 Dec 1959) (1200 16 Jan 1960) (1200 15 Feb 1960) (1200 16 Mar 1960) (0000 16 Apr 1960) (1200 16 May 1960) (0000 16 Jun 1960) (1200 16 Jul 1960) (1200 16 Aug 1960) (0000 16 Sep 1960) (1200 16 Oct 1960) (0000 16 Nov 1960) (0000 16 Dec 1960)] :grid
xi_rho: grid: /xi_rho (unitless) ordered (NaN) to (NaN) by NaN N= 397 pts :grid

Other Info

bufferwordsize: 8
CE: null
CS: null
datatype: doublearraytype
pointwidth: 1.0
units: PSU months days
history: Averaged over T2[16 Dec 1996 - 15 Dec 1997, 16 Dec 2007 - 15 Dec 2008]

Last updated: Thu, 27 Dec 2018 21:49:21 GMT

Data Views

	eta_rho	s_rho	T	xi_rho
$integral dT$ detrended-bfl [ $integral dT$ ( OLE2 ROMS-BACKUP salt ) climatology ] [ xi_rho eta_rho s_rho 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 xi_rho eta_rho s_rho T
Differentiate along xi_rho eta_rho s_rho T
Take differences along xi_rho eta_rho s_rho T