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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
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| lev | T | X | Y | |
 OLE2 ROMS[u
salt
v
temp
] | ||||
| OLE2 ROMS u[ X Y lev | T] | M | M | M | M |
|---|---|---|---|---|
| OLE2 ROMS u[ X Y lev | T] | M | M | M | M |
| OLE2 ROMS temp[ X Y lev | T] | M | M | M | M |
| OLE2 ROMS temp[ X Y lev | T] | M | M | M | 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
RMS (root mean square with mean *not* removed) over X Y lev T | X Y X lev X T Y lev Y T lev T | X Y lev X Y T X lev T Y lev T | X Y lev T |
RMSA (root mean square with mean removed) over X Y lev T | X Y X lev X T Y lev Y T lev T | X Y lev X Y T X lev T Y lev T | X Y lev T |
Maximum over X Y lev T | X Y X lev X T Y lev Y T lev T | X Y lev X Y T X lev T Y lev T | X Y lev T |
Minimum over X Y lev T | X Y X lev X T Y lev Y T lev T | X Y lev X Y T X lev T Y lev T | X Y lev T |
Detrend (best-fit-line) over X Y lev T | X Y X lev X T Y lev Y T lev T | X Y lev X Y T X lev T Y lev T | X Y lev T |
Note on units