served from IRI/LDEO Climate Data Library
IMD NCC1-2005 v4p0 stn: Number of stations data
Number of stations from IMD NCC1-2005 v4p0: IMD High Resolution (1°x1°) Daily Gridded Rainfall Data For the Indian Region 1951-2015 Version 4 (NCC1/2005).Independent Variables (Grids)
- Time (time)
- grid: /T (days since 1951-01-01 12:00:00) ordered (1 Jan 1951) to (30 Sep 2018) by 1.0 N= 24745 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (66.5E) to (100.5E) by 1.0 N= 35 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (6.5N) to (38.5N) by 1.0 N= 33 pts :grid
Other Info
- calendar
- standard
- datatype
- realarraytype
- missing_value
- 0.0
- pointwidth
- 1.0
- step
- 1.0
- units
- unitless
References
Rajeevan, M., J. Bhate, J. D. Kale, and B. Lal, 2005: Development of a high resolution daily gridded rainfall data for the Indian region. India Meteorological Department, Met. Monograph Climatology No. 22/2005, 26 pp.Rajeevan, M., J. Bhate, J. D. Kale, and B. Lal, 2006: A high resolution daily gridded rainfall for the Indian region: Analysis of break and active monsoon spells. Current Science, Vol. 91, No. 3, pp. 296-306.
Last updated: Wed, 13 Feb 2019 20:27:28 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 IMD NCC1-2005 v4p0 stn[ X Y | T] | 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 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