served from IRI/LDEO Climate Data Library
∫dT ∫dT [ IGOSS leetma d20C ] anomalies: Depth of 20C data
d20C int_dT int_dT Depth of 20C from IGOSS leetma: Pacific surface currents and equatorial thermocline depth.Independent Variables (Grids)
- Time
- grid: /T (months since 1960-01-01) ordered (0000 16 Dec 1979) to (0000 16 Nov 2008) by 1.0 N= 348 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (122.25E) to (71.25W) by 1.5 N= 112 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (35S) to (45N) by 1.0 N= 81 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- gridid
- 171677664
- maxncolor
- 254
- missing_value
- NaN
- positive
- down
- units
- 0.00694444444444444 meter year2
- history
- $integral dT$ $integral dT$ [ IGOSS leetma d20C ]
toS: regridded Z to NOAA NCEP EMC CMB Pacific monthly temp
- $integral dT$ $integral dT$ [ IGOSS leetma d20C ] climatology
- toS: regridded Z to NOAA NCEP EMC CMB Pacific monthly temp
Averaged over T2[Dec 1979 - Nov 1980, Dec 2007 - Nov 2008] minimum 0.0% data present
- toS: regridded Z to NOAA NCEP EMC CMB Pacific monthly temp
- $integral dT$ $integral dT$ [ IGOSS leetma d20C ]
Last updated: Mon, 12 Sep 2016 21:30:55 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 $integral dT$ $integral dT$ [ IGOSS leetma d20C ] anomalies[ 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
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