served from 129.236.110.25
∂X root mean sq ∂Y [ Princeton wspd ] : ∂X ∂Y Wind speed at 10 m data
∂X root mean sq ∂Y [ Princeton wspd ] .Independent Variables (Grids)
- Longitude (longitude)
- grid: /X (degree_east) periodic (0) to (0.5W) by 0.5 N= 720 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
- 3282.80635001174 meter radian-2 north second-1
- history
- Averaged over Y[89.75S, 89.75N] T[1 Jan 1948, 2400 30 Dec 2008] minimum 0.0% data present
Last updated: Fri, 27 Nov 2020 04:20:45 GMT
Data Views
Views
line plots
color bars
scatter| X | Z | |
 Princeton[prcp
tmin
tmax
wspd
] | ||
| grid: /X (degree_east) periodic (0.25E) to (0.25W) by 0.5 N= 720 pts :grid | O=-0.25 | |
|---|---|---|
| grid: /Y (degree_north) ordered (89.75S) to (89.75N) by 0.5 N= 360 pts :grid | ||
| 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 | ||
 $partialdiff sub X$ root mean sq $partialdiff sub Y$ [ Princeton wspd ] 0 m[ X Z |] | 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
- Differentiate along X
- Take differences along X
RMS (root mean square with mean *not* removed) over X |
RMSA (root mean square with mean removed) over X |
Maximum over X |
Minimum over X |
Detrend (best-fit-line) over X |
Note on units