served from 129.236.110.25
max ∫dT ∫dX ∫dT [ Princeton tmax ] : Maximum air temperature data
max ∫dT ∫dX ∫dT [ Princeton tmax ] .Independent Variables (Grids)
- Time (time)
- grid: /T (days since 1960-01-01 00:00:00) ordered (0000 31 Dec 1947) to (0000 1 Jan 2009) by 1.0 N= 22283 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 0.5 N= 359 pts :grid
- Depth
- grid: /Z (m) ordered [ (0)] :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- 2.00000004E20
- missing_value
- NaN
- pointwidth
- 0
- units
- 130288130.529676 degree_Kelvin radian east second2
- history
- max over X[0, 0]
Last updated: Fri, 27 Nov 2020 04:20:45 GMT
Data Views
Views
data as colors
data as contours| T | Y | Z | |
 Princeton[prcp
tmin
tmax
wspd
] | |||
 max $integral dT$ $integral dX$ $integral dT$ [ Princeton tmax ] 0 m[ Y Z | T] | 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 Y T
- Differentiate along Y T
- Take differences along Y T
RMS (root mean square with mean *not* removed) over Y T | Y T |
RMSA (root mean square with mean removed) over Y T | Y T |
Maximum over Y T | Y T |
Minimum over Y T | Y T |
Detrend (best-fit-line) over Y T | Y T |
Note on units