served from IRI/LDEO Climate Data Library
DASILVA SMD94 halfbyhalf climatology zdl: 10m / (Monin Obukov length) data
halfbyhalf climatology 10m / (Monin Obukov length) from DASILVA SMD94: a five-volume atlas series depicting the seasonal and yearly variations of the surface marine atmosphere over the global oceans.Independent Variables (Grids)
- Time
- grid: /T (months since 01-Jan) periodic (Jan) to (Dec) by 1.0 N= 12 pts :grid
- longitude
- grid: /X (degree_east) periodic (0.25E) to (0.25W) by 0.5 N= 720 pts :grid
- latitude
- grid: /Y (degree_north) ordered (89.75S) to (89.75N) by 0.5 N= 360 pts :grid
Other Info
- datatype
- realarraytype
- missing_value
- -1.00000000E10
- units
- unitless
- Version
- UWM-1.00 05/01/93
- history
- surface marine climatology 1945-89
References
A. da Silva, A. C. Young, S. Levitus. Atlas of Surface Marine Data 1994, Volume 1: Algorithms and Procedures, number 6, 1994
Last updated: Mon, 12 Sep 2016 21:11:58 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 DASILVA SMD94 halfbyhalf climatology zdl[ 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