served from 129.236.110.25
∂Y ∂T ∂X ∫dT [ Princeton prcp ] : ∂Y ∂T ∂X Total precipitation data
∂Y ∂T ∂X ∫dT [ Princeton prcp ] .Independent Variables (Grids)
- Time (time)
- grid: /T (days since 1960-01-01 00:00:00) ordered (1200 31 Dec 1947 - 1200 1 Jan 1948) to (1200 30 Dec 2008 - 1200 31 Dec 2008) by 1.0 N= 22281 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (0) to (0.5W) by 0.5 N= 720 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (89.25S) to (89.25N) by 0.5 N= 358 pts :grid
- Depth
- grid: /Z (m) ordered [ (0)] :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- file_missing_value
- 2.00000004E20
- missing_value
- NaN
- pointwidth
- 0
- units
- 3.79954438658766×10-05 meter radian-2 east second-1
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
] | ||||
 $partialdiff sub Y$ $partialdiff sub T$ $partialdiff sub X$ $integral dT$ [ Princeton prcp ] 0 m[ X Y Z | T] | M | M | M | M |
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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