max [ ∫dY ( NOAA NCDC ERSST version3b sst anomalies ) climatology ]: Extended reconstructed sea surface temperature data
sst sst int_dY int_dY Extended reconstructed sea surface temperature from NOAA NCDC ERSST version3b: ERSST.v3b: Extended Reconstructed Sea Surface Temperature Dataset, Verson 3b.
Independent Variables (Grids)
- Time (time)
- grid: /T (months since 01-Jan) periodic (Jan) to (Dec) by 1.0 N= 12 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (89S) to (89N) by 2.0 N= 90 pts :grid
- zlev
- grid: /zlev (meters) ordered [ (0.0)] :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- iridl:hasSemantics
- iridl:SeaSurfaceTemperature
- missing_value
- NaN
- pointwidth
- 1.0
- units
- 0.0174532925199433 degree_Kelvin radian north
- history
- NOAA NCDC ERSST version3b sst
Version 3b
- NOAA NCDC ERSST version3b sst climatology
- Version 3b
Averaged over T2[1854, 2024] minimum 0.0% data present
$integral dY$ [ NOAA NCDC ERSST version3b sst anomalies ] climatology- Averaged over T2[1854, 2024] minimum 0.0% data present
max [ $integral dY$ ( NOAA NCDC ERSST version3b sst anomalies ) climatology ]- max over X[0, 2W]
References
Smith_etal2008
Xue_etal2003
Last updated: Tue, 13 Aug 2024 08:17:43 GMT
Expires: Mon, 02 Sep 2024 00:00:00 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 Y
T
- Differentiate along Y
T
- Take differences along Y
T
Average over
Y
T
|
Y T
|
RMS (root mean square with mean *not* removed) over
Y
T
|
Y T
|
RMSA (root mean square with mean removed) over
Y
T
|
Y T
|
Maximum over
Y
T
|
Y T
|
Minimum over
Y
T
|
Y T
|
Detrend (best-fit-line) over
Y
T
|
Y T
|
Note on units