served from 129.236.110.25
mean mean ∫dT [ ∂T ( OLE2 ROMS-BACKUP temp ) anomalies ] : ∂T Temperatura Potencial data
mean mean ∫dT [ ∂T ( OLE2 ROMS-BACKUP temp ) anomalies ] .Independent Variables (Grids)
- s_rho
- grid: /s_rho (unitless) ordered (NaN) to (NaN) by NaN N= 32 pts :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
- degree_Celsius
- standard units*
- degree_Kelvin
- history
- mean $integral dT$ [ $partialdiff sub T$ ( OLE2 ROMS-BACKUP temp ) anomalies ]
- Averaged over T2[16 Jan 1997 - 15 Jan 1998, 16 Jan 2007 - 15 Jan 2008]
Averaged over eta_rho[NaN, NaN]
mean mean $integral dT$ [ $partialdiff sub T$ ( OLE2 ROMS-BACKUP temp ) anomalies ]- Averaged over T[0000 16 Jan 1997, 0000 16 Dec 2008]
- Averaged over T2[16 Jan 1997 - 15 Jan 1998, 16 Jan 2007 - 15 Jan 2008]
Last updated: Thu, 27 Dec 2018 21:49:21 GMT
Data Views
Views
data as colors
data as contours| s_rho | xi_rho | |
 mean mean $integral dT$ [ $partialdiff sub T$ ( OLE2 ROMS-BACKUP temp ) anomalies ] [ xi_rho s_rho |] | 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 s_rho
- Differentiate along xi_rho s_rho
- Take differences along xi_rho s_rho
RMS (root mean square with mean *not* removed) over xi_rho s_rho | xi_rho s_rho |
RMSA (root mean square with mean removed) over xi_rho s_rho | xi_rho s_rho |
Maximum over xi_rho s_rho | xi_rho s_rho |
Minimum over xi_rho s_rho | xi_rho s_rho |
Detrend (best-fit-line) over xi_rho s_rho | xi_rho s_rho |
Note on units