served from 129.236.110.25
root mean sq anom max [ T , max root mean sq anom ∫dT ( Princeton prcp ) ] : Time, Total precipitation data
root mean sq anom max [ T , max root mean sq anom ∫dT ( Princeton prcp ) ] . isIndependent Variables (Grids)
Other Info
- bufferwordsize
- 8
- calendar
- standard
- CE
- null
- CS
- null
- datatype
- doublearraytype
- fnname
- max
- gridid
- 177358464
- missing_value
- NaN
- pointwidth
- 0.0
- scale_max
- null
- scale_min
- null
- standard_name
- time
- units
- days since 1960-01-01 00:00
- standard units*
- 86400 ( seconds since 1960-01-01 00:00.000 )
- history
- max root mean sq anom $integral dT$ [ Princeton prcp ]
- Averaged over X[0.25E, 0.25W] minimum 0.0% data present
max over Y[89.75S, 89.75N]
root mean sq anom max [ T , max root mean sq anom $integral dT$ ( Princeton prcp ) ]- Averaged over T[1200 31 Dec 1947, 1200 31 Dec 2008] minimum 0.0% data present
- Averaged over X[0.25E, 0.25W] minimum 0.0% data present
Last updated: Fri, 27 Nov 2020 04:20:45 GMT
Data Views
 Princeton[prcp
tmin
tmax
wspd
] |
| grid: /Y (degree_north) ordered (89.75S) to (89.75N) by 0.5 N= 360 pts :grid |
 root mean sq anom max [ T , max root mean sq anom $integral dT$ ( Princeton prcp ) ] [ |] |
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
- Differentiate along
- Take differences along
RMS (root mean square with mean *not* removed) over
RMSA (root mean square with mean removed) over
Maximum over
Minimum over
Detrend (best-fit-line) over
Note on units