data: $integral dT$ [ $partialdiff sub T$ $integral dT$ detrended-bfl ( CAYAN Qnet ) anomalies ]

served from IRI/LDEO Climate Data Library

∫dT [ ∂_T ∫dT detrended-bfl ( CAYAN Qnet ) anomalies ]: ∂_T net heat flux data

Qnet Qnet Qnet Qnet adif adif int_dT partial_T partial_T partial_T ∂_T 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 Feb 1960) to (0000 1 Mar 1998) by 1.0 N= 458 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered [ (130E)] :grid
Latitude (latitude): grid: /Y (degree_north) ordered [ (20N)] :grid

Other Info

bufferwordsize

CE

null

CS

null

datatype

doublearraytype

file_missing_value

-99999.0

missing_value

NaN

units

0.0833333333333333 kilogram second^-3 year

history

$partialdiff sub T$ $integral dT$ detrended-bfl [ CAYAN Qnet ]
Cayan Net Heat Flux Derived from COADS

$partialdiff sub T$ $integral dT$ detrended-bfl [ CAYAN Qnet ] climatology

Cayan Net Heat Flux Derived from COADS
Averaged over T2[Feb 1960 - Jan 1961, Feb 1997 - Jan 1998] minimum 0.0% data present

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: Fri, 18 Sep 2015 18:39:06 GMT

Data Views

	T	X	Y
grid: /T (months since 1960-01-01) ordered (0000 1 Feb 1960) to (0000 1 Mar 1998) by 1.0 N= 458 pts :grid	M
$integral dT$ [ $partialdiff sub T$ $integral dT$ detrended-bfl ( CAYAN Qnet ) anomalies ] 130E 20N[ 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 T
Differentiate along T
Take differences along T