served from IRI/LDEO Climate Data Library
∂T ∫dX ∂X ∫dY [ IGOSS leetma v ] : ∂T ∂X meridional velocity data
v int_dY partial_X int_dX ∂T ∂X meridional velocity from IGOSS leetma: Pacific surface currents and equatorial thermocline depth.Independent Variables (Grids)
- Time
- grid: /T (months since 1960-01-01) ordered (16 Jan 1980 - 15 Feb 1980) to (16 Sep 2008 - 15 Oct 2008) by 1.0 N= 345 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 (35.5S) to (45.5N) by 1.0 N= 82 pts :grid
- Depth
- grid: /Z (m) ordered [ (5.0)] :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- missing_value
- NaN
- units
- 0.0020943951023932 meter radian east second-1 year-1
- history
- T: Feb 2005 to Oct 2008 appended from NOAA NCEP EMC CMB Pacific godas v
Last updated: Mon, 12 Sep 2016 21:30:56 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | Z | |
 $partialdiff sub T$ $integral dX$ $partialdiff sub X$ $integral dY$ [ IGOSS leetma v ] 5.0 m[ X Z | Y T] | M | 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