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root mean sq ∫dY [ NiMet ENACTS ENACTS_v1 ALL Temperature monthly c9120 tmean ] : Merged Station-Downscaled Reanalysis Mean Temperature Climatology 1991-2020 data
ENACTS_v1 ALL Temperature monthly c9120 tmean int_dY Merged Station-Downscaled Reanalysis Mean Temperature Climatology 1991-2020 from NiMet ENACTS: Enhancing National Climate Service Initiative.Independent Variables (Grids)
- Longitude (longitude)
- grid: /X (degree_east) ordered (2.4E) to (14.925E) by 0.03750001 N= 335 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (3.95625N) to (14.11875N) by 0.0375 N= 272 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- -99.0
- missing_value
- NaN
- units
- 0.0174532925199433 ( degree_Kelvin above 273.15 ) radian north
- history
- NiMet ENACTS ENACTS_v1 ALL Temperature monthly c9120 tmax
- Boxes with less than 100.0% dropped
Averaged over T2[1991, 2020] minimum 0.0% data present
root mean sq $integral dY$ [ NiMet ENACTS ENACTS_v1 ALL Temperature monthly c9120 tmean ]- Averaged over T[Jan, Dec] minimum 0.0% data present
- Boxes with less than 100.0% dropped
Last updated: Mon, 17 Feb 2025 14:29:37 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| X | Y | |
 root mean sq $integral dY$ [ NiMet ENACTS ENACTS_v1 ALL Temperature monthly c9120 tmean ] [ X Y |] | 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
- Differentiate along X Y
- Take differences along X Y
RMS (root mean square with mean *not* removed) over X Y | X Y |
RMSA (root mean square with mean removed) over X Y | X Y |
Maximum over X Y | X Y |
Minimum over X Y | X Y |
Detrend (best-fit-line) over X Y | X Y |
Note on units