served from IRI/LDEO Climate Data Library
RIHN aphrodite V1003R1 APHRO_RU_025deg rstn: ratio of 0.05 grid box contatining station(s) data
APHRO_RU_025deg ratio of 0.05 grid box contatining station(s) from RIHN aphrodite V1003R1: Asian precipitation products created by the Research Institute for Humanity and Nature and Meteorological Research Institute of Japan Meteorological Agency.Independent Variables (Grids)
- Time (time)
- grid: /T (days since 1960-01-01) ordered (1 Jan 1951) to (31 Dec 2007) by 1.0 N= 20819 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (15.125E) to (165.125W) by 0.25 N= 720 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (34.125N) to (83.875N) by 0.25 N= 200 pts :grid
Other Info
- datatype
- realarraytype
- missing_value
- -99.900002
- pointwidth
- 0
- units
- percent
- standard units*
- 0.01
References
Xie, P., A. Yatagai, M. Chen, T. Hayasaka, Y. Fukushima, C. Liu, and S. Yang (2007). A gauge-based analysis of daily precipitation over East Asia, Journal of Hydrometeorology, 8, 607-627.Yatagai, A. O. Arakawa, K. Kamiguchi, H. Kawamoto, M. I. Nodzu and A. Hamada (2009): A 44-year daily gridded precipitation dataset for Asia based on a dense network of rain gauges, SOLA, 5, 137-140, doi:10.2151/sola.2009-035.
Yatagai, A., K. Kamiguchi, O. Arakawa, A. Hamada, N. Yasutomi and A. Kitoh (2012): APHRODITE: Constructing a Long-term Daily Gridded Precipitation Dataset for Asia based on a Dense Network of Rain Gauges, Bull. Amer. Meteor. Soc., 93, 1401–1415. doi: http://dx.doi.org/10.1175/BAMS-D-11-00122.1
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 | |
 RIHN aphrodite V1003R1 APHRO_RU_025deg rstn[ 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