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∫dsl ∂X2 detrended-bfl detrended-bfl [ Ethiopia EthioSIS AWC ] : ∂X2 Available Water Capacity data
∫dsl ∂X2 detrended-bfl detrended-bfl [ Ethiopia EthioSIS AWC ] .Independent Variables (Grids)
- Soil Layer
- grid: /sl (cm) ordered [ (0.0) (5.0) (15.0) (30.0) (60.0) (100.0) (200.0)] :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (33.26423E) to (48.60844E) by 1.278684 N= 13 pts :grid
- X2
- grid: /X2 (degree_east) ordered [ (0.6393414W) (0.6293516W) (0.6193619W) ... (0.6293516E)] N= 128 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (3.384653N) to (14.89281N) by 1.278684 N= 10 pts :grid
- Y2
- grid: /Y2 (degree_north) periodic (0.634347S) to (0.634347N) by 0.009989716 N= 128 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- missing_value
- NaN
- units
- 0.00572957795130823 meter radian-1 east
Last updated: Wed, 01 Feb 2023 14:07:40 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| sl | X | X2 | Y | Y2 | |
 $integral dsl$ $partialdiff sub X2$ detrended-bfl detrended-bfl [ Ethiopia EthioSIS AWC ] [ X2 Y2 | sl X Y] | M | M | M | 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 X2 Y2 sl X Y
- Differentiate along X2 Y2 sl X Y
- Take differences along X2 Y2 sl X Y
RMS (root mean square with mean *not* removed) over X2 Y2 sl X Y | X2 Y2 X2 sl X2 X X2 Y Y2 sl Y2 X Y2 Y sl X sl Y X Y | X2 Y2 sl X2 Y2 X X2 Y2 Y X2 sl X X2 sl Y X2 X Y Y2 sl X Y2 sl Y Y2 X Y sl X Y | X2 Y2 sl X X2 Y2 sl Y X2 Y2 X Y X2 sl X Y Y2 sl X Y | X2 Y2 sl X Y |
RMSA (root mean square with mean removed) over X2 Y2 sl X Y | X2 Y2 X2 sl X2 X X2 Y Y2 sl Y2 X Y2 Y sl X sl Y X Y | X2 Y2 sl X2 Y2 X X2 Y2 Y X2 sl X X2 sl Y X2 X Y Y2 sl X Y2 sl Y Y2 X Y sl X Y | X2 Y2 sl X X2 Y2 sl Y X2 Y2 X Y X2 sl X Y Y2 sl X Y | X2 Y2 sl X Y |
Maximum over X2 Y2 sl X Y | X2 Y2 X2 sl X2 X X2 Y Y2 sl Y2 X Y2 Y sl X sl Y X Y | X2 Y2 sl X2 Y2 X X2 Y2 Y X2 sl X X2 sl Y X2 X Y Y2 sl X Y2 sl Y Y2 X Y sl X Y | X2 Y2 sl X X2 Y2 sl Y X2 Y2 X Y X2 sl X Y Y2 sl X Y | X2 Y2 sl X Y |
Minimum over X2 Y2 sl X Y | X2 Y2 X2 sl X2 X X2 Y Y2 sl Y2 X Y2 Y sl X sl Y X Y | X2 Y2 sl X2 Y2 X X2 Y2 Y X2 sl X X2 sl Y X2 X Y Y2 sl X Y2 sl Y Y2 X Y sl X Y | X2 Y2 sl X X2 Y2 sl Y X2 Y2 X Y X2 sl X Y Y2 sl X Y | X2 Y2 sl X Y |
Detrend (best-fit-line) over X2 Y2 sl X Y | X2 Y2 X2 sl X2 X X2 Y Y2 sl Y2 X Y2 Y sl X sl Y X Y | X2 Y2 sl X2 Y2 X X2 Y2 Y X2 sl X X2 sl Y X2 X Y Y2 sl X Y2 sl Y Y2 X Y sl X Y | X2 Y2 sl X X2 Y2 sl Y X2 Y2 X Y X2 sl X Y Y2 sl X Y | X2 Y2 sl X Y |
Note on units