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root mean sq anom [ ∫dX ∂Y ( ANACIM ENACTS version2 ALL dekadal climatologies tmax ) climatology ]: ∂Y Maximum Temperature data
version2 ALL dekadal climatologies tmax partial_Y int_dX int_dX ∂Y Maximum Temperature from ANACIM ENACTS: Enhancing National Climate Service initiative.Independent Variables (Grids)
- Time
- grid: /T (months since 1960-01-01) periodic (0000 1 Jan - 0000 11 Jan) to (0000 21 Dec - 0000 1 Jan) by 0.3333335 N= 36 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (17.60625W) to (11.19375W) by 0.0375 N= 172 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- colorscalename
- temp_colors
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- -99.0
- maxncolor
- 254
- missing_value
- NaN
- units
- degree_Celsius
- standard units*
- degree_Kelvin
- history
- $integral dX$ $partialdiff sub Y$ [ ANACIM ENACTS version2 ALL dekadal climatologies tmax ] climatology
- Averaged over T2[0.5, 1080.5] minimum 0.0% data present
Averaged over T2=1981 minimum 0.0% data present
root mean sq anom [ $integral dX$ $partialdiff sub Y$ ( ANACIM ENACTS version2 ALL dekadal climatologies tmax ) climatology ]- Averaged over Y[12.24375N, 16.78125N] minimum 0.0% data present
- Averaged over T2[0.5, 1080.5] minimum 0.0% data present
Last updated: Thu, 26 Oct 2023 14:58:08 GMT
Expires: Wed, 01 Nov 2023 00:00:00 GMT
Data Views
Views
data as colors
data as contours
line plots
color bars
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 T
- Differentiate along X T
- Take differences along X T
RMS (root mean square with mean *not* removed) over X T | X T |
RMSA (root mean square with mean removed) over X T | X T |
Maximum over X T | X T |
Minimum over X T | X T |
Detrend (best-fit-line) over X T | X T |
Note on units