data: detrended-bfl [ JONES landonly count ]

served from IRI/LDEO Climate Data Library

detrended-bfl [ JONES landonly count ]: station count per lat/lon box data

count station count per lat/lon box from JONES landonly: Land air temperature anomaly grids.

Independent Variables (Grids)

Time: grid: /T (months since 1960-01-01) ordered (Jan 1851) to (Dec 1993) by 1.0 N= 1716 pts :grid
longitude: grid: /X (degree_east) periodic (2.5E) to (2.5W) by 5.0 N= 72 pts :grid
latitude: grid: /Y (degree_north) ordered (87.5S) to (87.5N) by 5.0 N= 36 pts :grid

Other Info

bufferwordsize: 8
CE: null
CS: null
datatype: doublearraytype
missing_value: NaN
units: dimensionless

References

Jones, P. D., S. C. B. Raper, R. S. Bradley, H. F. Diaz, P. M. Kelly, and T. M. L. Wigley, 1986a: Northern Hemisphere surface air temperature variations, 1851--1984. J. Clim. Appl. Met., 25, 161--179.

Jones, P. D., S. C. B. Raper, R. S. Bradley, H. F. Diaz, P. M. Kelly, and T. M. L. Wigley, 1986b: Southern Hemisphere surface air temperature variations, 1851--1984. J. Clim. Appl. Met., 25, 1213--1230.

Last updated: Mon, 16 Feb 2015 21:51:22 GMT

Data Views

	T	X	Y
detrended-bfl [ JONES landonly count ][ X Y \| T]	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 X Y T
Differentiate along X Y T
Take differences along X Y T