served from IRI/LDEO Climate Data Library
detrended-bfl [ UEA CRU Jones HADCRUT2v temp ]: temperature_anomaly data
temp temperature_anomaly from UEA CRU Jones HADCRUT2v: Variance adjusted version of HadCRUT2 (superseded by HadCRUT3v).Independent Variables (Grids)
- Time
- grid: /T (months since 1870-1-1) ordered (Jan 1870) to (Dec 2005) by 1.0 N= 1632 pts :grid
- Longitude
- grid: /X (degree_east) periodic (177.5W) to (177.5E) by 5.0 N= 72 pts :grid
- Latitude
- grid: /Y (degree_north) ordered (87.5N) to (87.5S) by 5.0 N= 36 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- missing_value
- NaN
- units
- degree_Celsius
- standard units*
- degree_Kelvin
References
Jones_Moberg2003Jones_etal2001
Brohan_etal2006
Last updated: Mon, 12 Sep 2016 21:11:40 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 detrended-bfl [ UEA CRU Jones HADCRUT2v temp ][ 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