served from digilib.icpac.net
root mean sq ∂T root mean sq anom [ ENACTS version0 dekadal climatologies rfe_stddev climatology ] : ∂T Dekadal rainfall 1981-2010 standard deviation data
dekadal climatologies rfe_stddev rfe_stddev rfe_stddev partial_T ∂T Dekadal rainfall 1981-2010 standard deviation from ENACTS version0: version 0: CHIRPS-BLENDED and CRU.Independent Variables (Grids)
- Latitude (latitude)
- grid: /Y (degree_north) ordered (11.775S) to (23.125N) by 0.05 N= 699 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- colorscalename
- cmorph_dekad_colors
- CS
- null
- datatype
- doublearraytype
- maxncolor
- 254
- missing_value
- NaN
- units
- mm /month
- standard units*
- 0.012 meter year-1
- history
- ENACTS version0 dekadal climatologies rfe_stddev climatology
- Averaged over T2[18.5, 1062.5] minimum 0.0% data present
Averaged over T2=1981 minimum 0.0% data present
$partialdiff sub T$ root mean sq anom [ ENACTS version0 dekadal climatologies rfe_stddev climatology ]- Averaged over X[21.855E, 51.455E] minimum 0.0% data present
root mean sq $partialdiff sub T$ root mean sq anom [ ENACTS version0 dekadal climatologies rfe_stddev climatology ]- Averaged over T[0000 26 Dec - 0000 6 Jan, 0000 26 Dec - 0000 6 Jan] minimum 0.0% data present
- Averaged over T2[18.5, 1062.5] minimum 0.0% data present
Last updated: Mon, 28 Oct 2024 09:31:03 GMT
Expires: Fri, 11 Oct 2024 00:00:00 GMT
Data Views
Views
line plots
color bars
scatter
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
- Differentiate along Y
- Take differences along Y
RMS (root mean square with mean *not* removed) over Y |
RMSA (root mean square with mean removed) over Y |
Maximum over Y |
Minimum over Y |
Detrend (best-fit-line) over Y |
Note on units