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∂Y root mean sq detrended-bfl ∂X [ UEA CRU TS3p21 monthly dtr ] : ∂Y ∂X diurnal temperature range data
∂Y root mean sq detrended-bfl ∂X [ UEA CRU TS3p21 monthly dtr ] .Independent Variables (Grids)
- Time (time)
- grid: /T (months since 1960-01-01) ordered (Jan 1901) to (Dec 2012) by 1.0 N= 1344 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 0.5 N= 359 pts :grid
Other Info
- CE
- null
- correlation_decay_distance
- 750.0
- CS
- null
- datatype
- realarraytype
- file_missing_value
- 9.96920997E36
- missing_value
- NaN
- pointwidth
- 1
- units
- 3282.80635001174 degree_Kelvin radian-2 east
- history
- $partialdiff sub Y$ root mean sq detrended-bfl $partialdiff sub X$ [ UEA CRU TS3p21 monthly dtr ]
- Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for
Averaged over X[179.75E, 179.75E] minimum 0.0% data present
- Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for
References
Harris_etal2013Last updated: Fri, 26 Jul 2024 12:21:16 GMT
Data Views
Views
data as colors
data as contours| T | Y | |
 $partialdiff sub Y$ root mean sq detrended-bfl $partialdiff sub X$ [ UEA CRU TS3p21 monthly dtr ] [ Y | T] | 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 Y T
- Differentiate along Y T
- Take differences along 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