served from IRI/LDEO Climate Data Library
∫dT [ IGOSS leetma |u| ] climatology: surface speed data
leetma |u| |u| int_dT surface speed from IGOSS: Integrated Global Ocean Services System Products Bulletin.Independent Variables (Grids)
- Time
- grid: /T (months since 01-Jan) periodic (0000 1 Jan) to (0000 1 Dec) by 1.0 N= 12 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (123E) to (72W) by 1.5 N= 111 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (35S) to (45N) by 1.0 N= 81 pts :grid
- Depth
- grid: /Z (m) ordered [ (5.0)] :grid
Other Info
- CE
- null
- CI
- 50.0
- CS
- null
- datatype
- realarraytype
- fnname
- sqrt
- missing_value
- NaN
- units
- months
- standard units*
- 0.0833333333333333 year
- history
- $integral dT$ [ IGOSS leetma |u| ] climatology
- T: Feb 2005 to Oct 2008 appended from NOAA NCEP EMC CMB Pacific godas u
Averaged over T2[16 Dec 1979 - 15 Dec 1980, 16 Dec 2006 - 15 Dec 2007] minimum 0.0% data present
- T: Feb 2005 to Oct 2008 appended from NOAA NCEP EMC CMB Pacific godas u
Last updated: Wed, 13 Feb 2019 20:27:28 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | Z | |
 $integral dT$ [ IGOSS leetma |u| ] climatology 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