served from 129.236.110.25
OLE2 CAM3p1 HINDCAST OBS PRECSH: Shallow Convection precipitation rate data
OLE2 CAM3p1 HINDCAST OBS PRECSH.Independent Variables (Grids)
- member
- grid: /M (unitless) ordered (1.0) to (9.0) by 1.0 N= 9 pts :grid
- Time (time)
- grid: /T (months since 1960-01-01) ordered (Jan 1971) to (Dec 2010) by 1.0 N= 480 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (0) to (2.8125W) by 2.8125 N= 128 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (87.863S) to (87.863N) by 2.789302 N= 64 pts :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- pointwidth
- 1.0
- units
- mm /day
- standard units*
- 1.15740740740741×10-08 meter second-1
Last updated: Fri, 17 Jun 2016 14:57:32 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| M | T | X | Y | |
 OLE2 CAM3p1 HINDCAST OBS[PRECSL
TS
PRECL
TSMN
PRECSH
PRECC
TSMX
PRECSC
PRECT
] | ||||
| OLE2 CAM3p1 HINDCAST OBS PRECSH[ X Y | M T] | M | D | M | M |
|---|---|---|---|---|
| OLE2 CAM3p1 HINDCAST OBS TSMN[ X Y | M T] | M | M | M | M |
 OLE2 CAM3p1 HINDCAST OBS PRECSH[ X Y | M 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 M T
- Differentiate along X Y M T
- Take differences along X Y M T
RMS (root mean square with mean *not* removed) over X Y M T | X Y X M X T Y M Y T M T | X Y M X Y T X M T Y M T | X Y M T |
RMSA (root mean square with mean removed) over X Y M T | X Y X M X T Y M Y T M T | X Y M X Y T X M T Y M T | X Y M T |
Maximum over X Y M T | X Y X M X T Y M Y T M T | X Y M X Y T X M T Y M T | X Y M T |
Minimum over X Y M T | X Y X M X T Y M Y T M T | X Y M X Y T X M T Y M T | X Y M T |
Detrend (best-fit-line) over X Y M T | X Y X M X T Y M Y T M T | X Y M X Y T X M T Y M T | X Y M T |
Note on units