data: OLE2 ROMS temp

served from 129.236.110.25

OLE2 ROMS temp: Temperatura Potencial data

OLE2 ROMS temp.

Independent Variables (Grids)

lev: grid: /lev (meters) ordered [ (0.0) (2.5) (5.0) (10.0) (15.0) (25.0) (50.0) (75.0) (100.0) (125.0) (150.0) (175.0)] :grid
Time (time): grid: /T (months since 1960-01-01) ordered (Jan 1997) to (Dec 2008) by 1.0 N= 144 pts :grid
Longitude: grid: /X (degree_east) ordered (100W) to (56W) by 0.1111111 N= 397 pts :grid
Latitude: grid: /Y (degree_north) ordered [ (10S) (9.890577S) (9.781117S) ... (25.00823N)] N= 324 pts :grid

Other Info

datatype: realarraytype
pointwidth: 1.0
units: degreeC
standard units*: degree_Kelvin

Last updated: Thu, 27 Dec 2018 23:07:12 GMT

Data Views

	lev	T	X	Y
grid: /X (degree_east) ordered (100W) to (56W) by 0.1111111 N= 397 pts :grid			M
grid: /Y (degree_north) ordered [ (10S) (9.890577S) (9.781117S) ... (25.00823N)] N= 324 pts :grid				M
grid: /lev (meters) ordered [ (0.0) (2.5) (5.0) (10.0) (15.0) (25.0) (50.0) (75.0) (100.0) (125.0) (150.0) (175.0)] :grid	M
grid: /T (months since 1960-01-01) ordered (Jan 1997) to (Dec 2008) by 1.0 N= 144 pts :grid		M
OLE2 ROMS temp[ X Y lev \| 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 X Y lev T
Differentiate along X Y lev T
Take differences along X Y lev T