served from IRI/LDEO Climate Data Library
DASILVA SMD94 halfbyhalf climatology longrad: outgoing longwave radiation data
halfbyhalf climatology outgoing longwave radiation 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
- W /m2
- Version
- UWM-1.00 05/01/93
- standard units*
- kilogram second-3
- history
- surface marine climatology 1945-89
References
daSilva_etal1994Last updated: Mon, 12 Sep 2016 21:11:57 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 longrad[ 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