served from IRI/LDEO Climate Data Library
∫dX ∫dT [ NOAA NCEP EMC CMB Pacific weekly D20eq ] : Depth of 20C data
weekly D20eq int_dT Depth of 20C from NOAA NCEP EMC CMB Pacific: Pacific Ocean Hindcast data derived from a model-based ocean analysis system.Independent Variables (Grids)
- Time
- grid: /T (julian_day) unordered [ (0000 29 Dec 1996) (0000 5 Jan 1997) (0000 12 Jan 1997) ... (0000 2 Nov 2008)] N= 814 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (121.5E) to (70.5W) by 1.5 N= 113 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered [ (0)] :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- gridid
- 171492200
- maxncolor
- 254
- missing_value
- NaN
- positive
- down
- units
- 1507.9644737231 meter radian east second
- history
- $integral dX$ $integral dT$ [ NOAA NCEP EMC CMB Pacific weekly D20eq ]
- toS: regridded Z to NOAA NCEP EMC CMB Pacific weekly temp 0
T: 6-12 Feb 2005 to 1200 29 Oct 2008 appended from NOAA NCEP EMC CMB Pacific godas D20eq
- toS: regridded Z to NOAA NCEP EMC CMB Pacific weekly temp 0
References
Behringer_etal1998Ji_etal1995
Ji_Smith1995
Last updated: Mon, 12 Sep 2016 21:28:51 GMT
Data Views
Views
data as colors
data as contours
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
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