served from IRI/LDEO Climate Data Library
∂Y ∫dX [ UEA CRU TS2p1 monthly dtr ] : ∂Y diurnal temperature range data
monthly dtr int_dX ∂Y diurnal temperature range from UEA CRU TS2p1: Mean surface climate data over global land areas, including tercile and percentile data.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 1960-01-01) ordered (Jan 1901) to (Dec 2002) by 1.0 N= 1224 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (180W) to (180) by 0.5 N= 721 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 0.5 N= 359 pts :grid
Other Info
- datatype
- realarraytype
- file_missing_value
- -99.900002
- missing_value
- NaN
- units
- degree_Celsius
- standard units*
- degree_Kelvin
References
Mitchell_Jones2005Last updated: Mon, 12 Sep 2016 21:34:09 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 $partialdiff sub Y$ $integral dX$ [ UEA CRU TS2p1 monthly dtr ] [ X Y | T] | M | M | M |
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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 Y T
- Differentiate along X Y T
- Take differences along X Y T
RMS (root mean square with mean *not* removed) over X Y T | X Y X T Y T | X Y T |
RMSA (root mean square with mean removed) over X Y T | X Y X T Y T | X Y T |
Maximum over X Y T | X Y X T Y T | X Y T |
Minimum over X Y T | X Y X T Y T | X Y T |
Detrend (best-fit-line) over X Y T | X Y X T Y T | X Y T |
Note on units