data: $integral dlon$ [ UEA CRU TS4p0 monthly pet ]

served from 129.236.110.25

∫dlon [ UEA CRU TS4p0 monthly pet ]: potential evapotranspiration data

∫dlon [ UEA CRU TS4p0 monthly pet ].

Independent Variables (Grids)

lat (latitude): grid: /lat (degree_north) ordered (89.75S) to (89.75N) by 0.5 N= 360 pts :grid
lon (longitude): grid: /lon (degree_east) ordered (180W) to (180) by 0.5 N= 721 pts :grid
time (time): grid: /time (months since 1960-01-01) ordered (Jan 1901) to (Dec 2015) by 1.0 N= 1380 pts :grid

Other Info

bufferwordsize: 8
correlation_decay_distance: -999.0
datatype: doublearraytype
file_missing_value: 9.96920997E36
missing_value: NaN
standard_name: water_potential_evaporation_flux
units: 2.02005700462307×10^-10 meter radian east second^-1
history: Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for

References

Harris_etal2013

Last updated: Wed, 17 Jan 2024 21:25:22 GMT

Data Views

	lat	lon	time
UEA CRU TS4p0 monthly[dtr cld tmp wet pet tmn vap tmx frs pre ]
UEA CRU TS4p0 monthly vap[ lon lat \| time]	M	O=-0.25	M
UEA CRU TS4p0 monthly wet[ lon lat \| time]	M	O=-0.25	M
$integral dlon$ [ UEA CRU TS4p0 monthly pet ][ lon lat \| time]	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 lon lat time
Differentiate along lon lat time
Take differences along lon lat time