served from IRI/LDEO Climate Data Library
∂T [ WEARE MONTHLY dqsa ] anomalies: ∂T sea-air specific humidity difference data
MONTHLY dqsa partial_T ∂T sea-air specific humidity difference from WEARE: Marine climate atlas of the tropical Pacific Ocean.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 1960-01-01) ordered (16 Jan 1957 - 15 Feb 1957) to (16 Nov 1976 - 15 Dec 1976) by 1.0 N= 239 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (112.5E) to (72.5W) by 5.0 N= 36 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (37.5S) to (27.5N) by 5.0 N= 14 pts :grid
Other Info
- CE
- null
- CS
- null
- file_missing_value
- 1.00000002E30
- missing_value
- NaN
- units
- 0.012 year-1
- history
- $partialdiff sub T$ [ WEARE MONTHLY dqsa ]
Weare averaged surface data
- $partialdiff sub T$ [ WEARE MONTHLY dqsa ] climatology
- Weare averaged surface data
Averaged over T2[16 Jan 1957 - 15 Jan 1958, 16 Jan 1975 - 15 Jan 1976] minimum 0.0% data present
- Weare averaged surface data
- $partialdiff sub T$ [ WEARE MONTHLY dqsa ]
References
Weare_etal1980Weare_etal1981
Last updated: Mon, 12 Sep 2016 21:13:53 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 $partialdiff sub T$ [ WEARE MONTHLY dqsa ] anomalies[ Y X | 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 Y X T
- Differentiate along Y X T
- Take differences along Y X T
RMS (root mean square with mean *not* removed) over Y X T | Y X Y T X T | Y X T |
RMSA (root mean square with mean removed) over Y X T | Y X Y T X T | Y X T |
Maximum over Y X T | Y X Y T X T | Y X T |
Minimum over Y X T | Y X Y T X T | Y X T |
Detrend (best-fit-line) over Y X T | Y X Y T X T | Y X T |
Note on units