∂T root mean sq ∂X [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ] : ∂T ∂X Sea Surface Temperature data
monthly sst sst partial_X partial_X
∂T ∂X 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 (180W) to (179E) by 1.0 N= 360 pts :grid
Other Info
- CE
- null
- colorscalename
- sstcolorscale
- CS
- null
- datatype
- realarraytype
- PLOTCOAST
- 1
- units
- 687.549354156988 degree_Kelvin radian-1 east year-1
- history
- $partialdiff sub X$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ]
- Monthly mean sea surface temperature (blended from ship, buoy and bias-corrected satellite data).
$partialdiff sub T$ root mean sq $partialdiff sub X$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv1 monthly sst ] - Averaged over Y[90S, 90N]
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
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
T
- Differentiate along X
T
- Take differences along X
T
Average over
X
T
|
X T
|
RMS (root mean square with mean *not* removed) over
X
T
|
X T
|
RMSA (root mean square with mean removed) over
X
T
|
X T
|
Maximum over
X
T
|
X T
|
Minimum over
X
T
|
X T
|
Detrend (best-fit-line) over
X
T
|
X T
|
Note on units