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∂T ∫dT root mean sq [ UEA CRU TS3p21 monthly vap anomalies ] : ∂T vapour pressure data
∂T ∫dT root mean sq [ UEA CRU TS3p21 monthly vap anomalies ] .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
- Longitude (longitude)
- grid: /X (degree_east) periodic (179.75W) to (179.75E) by 0.5 N= 720 pts :grid
Other Info
- CE
- null
- correlation_decay_distance
- 1000.0
- CS
- null
- datatype
- realarraytype
- file_missing_value
- 9.96920997E36
- missing_value
- NaN
- pointwidth
- 1
- standard_name
- water_vapor_pressure
- units
- hPa
- standard units*
- 100 kilogram meter-1 second-2
- history
- UEA CRU TS3p21 monthly vap
Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for
- UEA CRU TS3p21 monthly vap climatology
- Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for
Averaged over T2[1901, 2012] minimum 0.0% data present
- Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for
- Averaged over Y[90S, 90N] minimum 0.0% data present
- UEA CRU TS3p21 monthly vap
References
Harris_etal2013Last updated: Fri, 26 Jul 2024 12:21:16 GMT
Data Views
Views
data as colors
data as contours| T | X | |
 $partialdiff sub T$ $integral dT$ root mean sq [ UEA CRU TS3p21 monthly vap anomalies ] [ X | 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 X T
- Differentiate along X T
- Take differences along X T
RMS (root mean square with mean *not* removed) over X T | X T |
RMSA (root mean square with mean removed) over X T | X T |
Maximum over X T | X T |
Minimum over X T | X T |
Detrend (best-fit-line) over X T | X T |
Note on units