served from IRI/LDEO Climate Data Library
root mean sq detrended-bfl root mean sq ∂T ∂Y [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ] : ∂T ∂Y Sea Surface Temperature data
monthly sst sst partial_Y partial_T partial_T adif ∂T ∂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). isIndependent Variables (Grids)
Other Info
- bufferwordsize
- 8
- CE
- null
- colorscalename
- sstcolorscale
- CS
- null
- datatype
- doublearraytype
- PLOTCOAST
- 1
- units
- 687.549354156988 degree_Kelvin radian-1 north year-1
- history
- $partialdiff sub T$ $partialdiff sub Y$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ]
- Monthly mean sea surface temperature (blended from ship, buoy and bias-corrected satellite data).
detrended-bfl root mean sq $partialdiff sub T$ $partialdiff sub Y$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ]- Averaged over Y[89.5S, 89.5N] T[16 Dec 1989 - 15 Jan 1990, 16 Oct 1999 - 15 Nov 1999]
root mean sq detrended-bfl root mean sq $partialdiff sub T$ $partialdiff sub Y$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ]- Averaged over X[180W, 180]
References
R. W. Reynolds, T. M. Smith. Improved global sea surface temperature analyses.. J. Climate 7, 1994
Last updated: Mon, 12 Sep 2016 21:13:54 GMT
Data Views
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
- Differentiate along
- Take differences along
RMS (root mean square with mean *not* removed) over
RMSA (root mean square with mean removed) over
Maximum over
Minimum over
Detrend (best-fit-line) over
Note on units