data: $integral dX$ $integral dT$ detrended-bfl $integral dY$ [ CAYAN Qnet ]

served from IRI/LDEO Climate Data Library

∫dX ∫dT detrended-bfl ∫dY [ CAYAN Qnet ] : net heat flux data

Qnet Qnet int_dY adif int_dT net heat flux from CAYAN: Heat flux and irradiance data analysis of COADS from Cayan of Scripps.

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (0000 1 Jan 1946) to (0000 1 Apr 1998) by 1.0 N= 628 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (2.5E) to (2.5E) by 5.0 N= 73 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (70N) to (40S) by 5.0 N= 23 pts :grid

Other Info

bufferwordsize: 8
CE: null
CS: null
datatype: doublearraytype
file_missing_value: -99999.0
missing_value: NaN
units: 2.53847849822257×10^-05 kilogram radian² east second^-3 year
history: Cayan Net Heat Flux Derived from COADS

References

Cayan, D., 1992: Latent and Sensible Heat Flux Anomalies over the Northern Oceans: The Connection to Monthly Atmospheric Circulation. J. Climate, 5, 354-369.

Last updated: Wed, 13 Feb 2019 20:27:28 GMT

Data Views

	T	X	Y
$integral dX$ $integral dT$ detrended-bfl $integral dY$ [ CAYAN Qnet ] [ 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