data: $integral dY$ detrended-bfl $partialdiff sub Y$ [ NOAA NCEP EMC CMB GLOBAL Reyn

served from IRI/LDEO Climate Data Library

∫dY detrended-bfl ∂_Y [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ] : ∂_Y Sea Surface Temperature data

monthly sst sst partial_Y adif adif ∂_Y Sea Surface Temperature from NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1: Sea surface temperature fields blended from ship, buoy and bias-corrected satellite data (Reynolds and Smith 1994).

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (16 Dec 1989 - 15 Jan 1990) to (16 Oct 1999 - 15 Nov 1999) by 1.0 N= 119 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (179.5W) to (179.5E) by 1.0 N= 360 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 1.0 N= 180 pts :grid

Other Info

bufferwordsize

CE

null

colorscalename

sstcolorscale

CS

null

datatype

doublearraytype

PLOTCOAST

units

degree_Celsius

standard units*

degree_Kelvin

history

$integral dY$ detrended-bfl $partialdiff sub Y$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ]

Monthly mean sea surface temperature (blended from ship, buoy and bias-corrected satellite data).

References

R. W. Reynolds, T. M. Smith. Improved global sea surface temperature analyses.. J. Climate 7, 1994

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

Data Views

	T	X	Y
$integral dY$ detrended-bfl $partialdiff sub Y$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ] [ 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