served from IRI/LDEO Climate Data Library
detrended-bfl ∂T ∂T [ ∂T T ] : ∂T ∂T ∂T Time data
detrended-bfl ∂T ∂T [ ∂T T ] .Independent Variables (Grids)
- Time (time)
- grid: /T (days since 1948-01-01 12:00:00) ordered (3 Jan 1948) to (17 May 2024) by 1.0 N= 27895 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- CS
- null
- datatype
- doublearraytype
- gridid
- 177357904
- scale_max
- null
- scale_min
- null
- standard_name
- time
- units
- 1.33959190672154×10-10 second-2
Last updated: Tue, 21 May 2024 13:55:30 GMT
Expires: Wed, 22 May 2024 13:40:00 GMT
Data Views
Views
line plots
color bars
scatter| T | X | Y | |
 $integral dT$ [ NOAA NCEP-NCAR CDAS-1 DAILY Intrinsic total_air_column PWAT ][ X Y | T] | S | M | M |
|---|---|---|---|
| grid: /T (days since 1948-01-01 12:00:00) ordered (1 Jan 1948) to (19 May 2024) by 1.0 N= 27899 pts :grid | S | ||
| grid: /Y (degree_north) ordered (88.75N) to (88.75S) by 2.5 N= 72 pts :grid | M | ||
| $partialdiff sub T$ T[ T |] | O=0.5 | ||
 detrended-bfl $partialdiff sub T$ $partialdiff sub T$ [ $partialdiff sub T$ T ] [ T |] | 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 T
- Differentiate along T
- Take differences along T
RMS (root mean square with mean *not* removed) over T |
RMSA (root mean square with mean removed) over T |
Maximum over T |
Minimum over T |
Detrend (best-fit-line) over T |
Note on units