served from 129.236.110.25
∫dX max [ ( Princeton tmax ) , max ( Princeton wspd ) ] : Maximum air temperature, Wind speed at 10 m data
∫dX max [ ( Princeton tmax ) , max ( Princeton wspd ) ] .Independent Variables (Grids)
- Time (time)
- grid: /T (days since 1960-01-01 00:00:00) ordered (0000 1 Jan 1948) to (0000 31 Dec 2008) by 1.0 N= 22281 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (0) to (0) by 0.5 N= 721 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (89.75S) to (89.75N) by 0.5 N= 360 pts :grid
- Depth
- grid: /Z (m) ordered [ (0)] :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- 2.00000004E20
- fnname
- max
- missing_value
- NaN
- pointwidth
- 0
- units
- 0.0174532925199433 ( degree_Kelvin above 273.15 ) radian east
- history
- max over Y[89.75S, 89.75N]
Last updated: Fri, 27 Nov 2020 04:20:45 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | Z | |
 Princeton[prcp
tmin
tmax
wspd
] | ||||
 $integral dX$ max [ ( Princeton tmax ) , max ( Princeton wspd ) ] 0 m[ X | Y T Z] | 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 T
- Differentiate along X Y T
- Take differences along X Y T
RMS (root mean square with mean *not* removed) over X Y T | X Y X T Y T | X Y T |
RMSA (root mean square with mean removed) over X Y T | X Y X T Y T | X Y T |
Maximum over X Y T | X Y X T Y T | X Y T |
Minimum over X Y T | X Y X T Y T | X Y T |
Detrend (best-fit-line) over X Y T | X Y X T Y T | X Y T |
Note on units