served from data-library.gov.ls
root mean sq ∂X ∫dY [ Lesotho ENACTS ALL monthly temperature tmax anomalies ] : ∂X Maximum Temperature data
ALL monthly temperature tmax tmax int_dY partial_X ∂X Maximum Temperature from Lesotho ENACTS: Enhancing National Climate Service initiative.Independent Variables (Grids)
- Longitude (longitude)
- grid: /X (degree_east) ordered (26.94375E) to (29.56875E) by 0.03750003 N= 71 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (30.80625S) to (28.40625S) by 0.03749999 N= 65 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- -99.0
- missing_value
- NaN
- units
- degree_Celsius
- standard units*
- degree_Kelvin
- history
- Lesotho ENACTS ALL monthly temperature tmax
Boxes with less than 100.0% dropped
- Lesotho ENACTS ALL monthly temperature tmax climatology
- Boxes with less than 100.0% dropped
Averaged over T2[1961, 2020] minimum 0.0% data present
- Boxes with less than 100.0% dropped
- Averaged over T[Jan 1961, Dec 2020] minimum 0.0% data present
- Lesotho ENACTS ALL monthly temperature tmax
Last updated: Wed, 09 Mar 2022 20:30:18 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts
line plots
color bars| X | Y | |
 root mean sq $partialdiff sub X$ $integral dY$ [ Lesotho ENACTS ALL monthly temperature tmax anomalies ] [ 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