served from IRI/LDEO Climate Data Library
NOAA NCEP EMC CMB T40 PressureLevel Div: divergence data
T40 PressureLevel divergence from NOAA NCEP EMC CMB: Climate Modeling Branch.Independent Variables (Grids)
- M
- grid: /M (unitless) ordered (1.0) to (13.0) by 1.0 N= 13 pts :grid
- pressure
- grid: /P (mb) ordered [ (1000.0) (925.0) (850.0) (700.0) (600.0) (500.0) (400.0) (300.0) (250.0) (200.0) (150.0) (100.0) (70.0) (50.0) (30.0) (20.0) (10.0)] :grid
- Time (time)
- grid: /T (months since 1960-01-01) ordered (Feb 1950) to (Feb 1995) by 1.0 N= 541 pts :grid
- Longitude
- grid: /X (degree_east) periodic (0) to (2.8125W) by 2.8125 N= 128 pts :grid
- Latitude
- grid: /Y (degree_north) ordered [ (87.86384N) (85.09651N) (82.3129N) (79.52561N) (76.73689N) (73.94751N) (71.15775N) (68.36775N) (65.57761N) (62.78734N) (59.99702N) (57.20663N) (54.41619N) (51.62573N) (48.83524N) (46.04472N) (43.2542N) (40.46365N) (37.67308N) (34.88252N) (32.09194N) (29.30136N) (26.51077N) (23.72017N) (20.92957N) (18.13897N) (15.34836N) (12.55776N) (9.767144N) (6.976533N) (4.18592N) (1.395307N) (1.395307S) (4.18592S) (6.976533S) (9.767144S) (12.55776S) (15.34836S) (18.13897S) (20.92957S) (23.72017S) (26.51077S) (29.30136S) (32.09194S) (34.88252S) (37.67308S) (40.46365S) (43.2542S) (46.04472S) (48.83524S) (51.62573S) (54.41619S) (57.20663S) (59.99702S) (62.78734S) (65.57761S) (68.36775S) (71.15775S) (73.94751S) (76.73689S) (79.52561S) (82.3129S) (85.09651S) (87.86384S)] :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- missing_value
- NaN
- units
- unitless
- history
- toS: regridded Z to NOAA NCEP EMC CMB T40 Intrinsic P
Last updated: Fri, 18 Sep 2015 18:39:07 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| M | P | T | X | Y | |
 NOAA NCEP EMC CMB T40 PressureLevel Div[ X Y P | M T] | M | M | M | M | M |
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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 P M T
- Differentiate along X Y P M T
- Take differences along X Y P M T
RMS (root mean square with mean *not* removed) over X Y P M T | X Y X P X M X T Y P Y M Y T P M P T M T | X Y P X Y M X Y T X P M X P T X M T Y P M Y P T Y M T P M T | X Y P M X Y P T X Y M T X P M T Y P M T | X Y P M T |
RMSA (root mean square with mean removed) over X Y P M T | X Y X P X M X T Y P Y M Y T P M P T M T | X Y P X Y M X Y T X P M X P T X M T Y P M Y P T Y M T P M T | X Y P M X Y P T X Y M T X P M T Y P M T | X Y P M T |
Maximum over X Y P M T | X Y X P X M X T Y P Y M Y T P M P T M T | X Y P X Y M X Y T X P M X P T X M T Y P M Y P T Y M T P M T | X Y P M X Y P T X Y M T X P M T Y P M T | X Y P M T |
Minimum over X Y P M T | X Y X P X M X T Y P Y M Y T P M P T M T | X Y P X Y M X Y T X P M X P T X M T Y P M Y P T Y M T P M T | X Y P M X Y P T X Y M T X P M T Y P M T | X Y P M T |
Detrend (best-fit-line) over X Y P M T | X Y X P X M X T Y P Y M Y T P M P T M T | X Y P X Y M X Y T X P M X P T X M T Y P M Y P T Y M T P M T | X Y P M X Y P T X Y M T X P M T Y P M T | X Y P M T |
Note on units