served from IRI/LDEO Climate Data Library
∫dT ∂Y [ IGOSS nmc Reyn_SmithOIv2 weekly ssta ] : ∂Y Sea Surface Temperature Anomaly data
weekly ssta ssta ssta partial_Y ∂Y Sea Surface Temperature Anomaly from IGOSS nmc Reyn_SmithOIv2: SST fields updated from version 1 with more COADS data, new sea-ice to SST conversion algorithm, and 1971-2000 climatology.Independent Variables (Grids)
- Time
- grid: /T (julian_day) ordered [ (0000 5 Nov 1981) (0000 12 Nov 1981) (0000 19 Nov 1981) ... (0000 5 Feb 2023)] N= 2154 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (1.5E) to (0.5E) by 1.0 N= 360 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (89S) to (89N) by 1.0 N= 179 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- colorscalename
- sstacolorscale
- CS
- null
- datatype
- doublearraytype
- maxncolor
- 254
- missing_value
- NaN
- PLOTCOAST
- 1
- units
- 4950355.34993031 degree_Kelvin radian-1 north second
- history
- NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology sst
- Averaged over T[Jan, Dec] minimum 0.0% data present
T regridded on NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology sst
Boxes with less than 0.0% dropped
- Averaged over T[Jan, Dec] minimum 0.0% data present
References
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Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts
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
RMS (root mean square with mean *not* removed) over X Y T | X Y X T Y T | X Y T |
RMSA (root mean square with mean removed) over X Y T | X Y X T Y T | X Y T |
Maximum over X Y T | X Y X T Y T | X Y T |
Minimum over X Y T | X Y X T Y T | X Y T |
Detrend (best-fit-line) over X Y T | X Y X T Y T | X Y T |
Note on units