mean ∫dT [ ∫dY ( UCSB CHIRPS v1p8 dekad prcp climatology ) anomalies ] : precipitation data
CHIRPS v1p8 dekad prcp prcp int_dY int_dY int_dT precipitation from UCSB: UC Santa Barbara.
Independent Variables (Grids)
- Time
- grid: /T (months since 1960-01-01) ordered (0000 1 Jan 1960) to (0000 1 Jan 1961) by 0.3333335 N= 37 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (50N) to (50S) by 0.05 N= 2001 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- colorscalename
- prcp_dekadrate_max600_smooth
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- -9999.0
- maxncolor
- 254
- missing_value
- NaN
- standard_name
- lwe_precipitation_rate
- units
- 1.45444104332861×10-06 meter radian north year
- history
- $integral dY$ [ UCSB CHIRPS v1p8 dekad prcp climatology ]
Averaged over T2[1981, 2357 30 Dec 2023 - 2357 30 Dec 2024] minimum 0.0% data present
- $integral dY$ [ UCSB CHIRPS v1p8 dekad prcp climatology ] climatology
- Averaged over T2[1981, 2357 30 Dec 2023 - 2357 30 Dec 2024] minimum 0.0% data present
Averaged over T2=0000 1 Jan 1960 - 0000 1 Jan 1961 minimum 0.0% data present
mean $integral dT$ [ $integral dY$ ( UCSB CHIRPS v1p8 dekad prcp climatology ) anomalies ] - Averaged over X[180W, 180] minimum 0.0% data present
References
Funk_etal2014
Last updated: Thu, 02 Nov 2023 07:43:25 GMT
Expires: Tue, 01 Jul 2025 00:00:00 GMT
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 Y
T
- Differentiate along Y
T
- Take differences along Y
T
Average over
Y
T
|
Y T
|
RMS (root mean square with mean *not* removed) over
Y
T
|
Y T
|
RMSA (root mean square with mean removed) over
Y
T
|
Y T
|
Maximum over
Y
T
|
Y T
|
Minimum over
Y
T
|
Y T
|
Detrend (best-fit-line) over
Y
T
|
Y T
|
Note on units