CMORPH 0.25 degree 3-hourly Global Precipitation Estimates from Passive Microwave and Infrared DataEntry ID: GES_DISC_CMORPHRAIN_V1.0
Abstract: NOAA CPC Morphing Technique ("CMORPH")
Grid Resolution: 0.25 degrees lat/lon
Temporal Resolution: 3-hourly
Domain: Global (60N - 60S)
Period of Record: December 3, 2002 to present
Reference: Joyce, R. J., J. E. Janowiak, P. A. Arkin, and P. Xie, 2004: CMORPH: A method that produces global precipitation estimates from passive microwave and infrared data ... at high spatial and temporal resolution.. J. Hydromet., 5, 487-503.
CMORPH (CPC MORPHing technique) produces global precipitation analyses at very high spatial and temporal resolution. This technique uses precipitation estimates that have been derived from low orbiter satellite microwave observations exclusively, and whose features are transported via spatial propagation information that is obtained entirely from geostationary satellite IR data. At present we incorporate precipitation estimates derived from the passive microwaves aboard the DMSP 13, 14 & 15 (SSM/I), the NOAA-15, 16, 17 & 18 (AMSU-B), and AMSR-E and TMI aboard NASA's Aqua and TRMM spacecraft, respectively. These estimates are generated by algorithms of Ferraro (1997) for SSM/I, Ferraro et al. (2000) for AMSU-B and Kummerow et al. (2001) for TMI. Note that this technique is not a precipitation estimation algorithm but a means by which estimates from existing microwave rainfall algorithms can be combined. Therefore, this method is extremely flexible such that any precipitation estimates from any microwave satellite source can be incorporated.
With regard to spatial resolution, although the preciptation estimates are available on a grid with a spacing of 8 km (at the equator), the resolution of the individual satellite-derived estimates is coarser than that - more on the order of 12 x 15 km or so. The finer "resolution" is obtained via interpolation.
In effect, IR data are used as a means to transport the microwave-derived precipitation features during periods when microwave data are not available at a location. Propagation vector matrices are produced by computing spatial lag correlations on successive images of geostationary satellite IR which are then used to propagate the microwave derived precipitation estimates. This process governs the movement of the precipitation features only. At a given location, the shape and intensity of the precipitation features in the intervening half hour periods between microwave scans are determined by performing a time-weighting interpolation between microwave-derived features that have been propagated forward in time from the previous microwave observation and those that have been propagated backward in time from the following microwave scan. We refer to this latter step as "morphing" of the features.
Other Citation Details:
Joyce, R. J., J. E. Janowiak, P. A. Arkin, and P. Xie, 2004: CMORPH: A method that produces global precipitation estimates from passive microwave and infrared data at high spatial and temporal resolution.. J. Hydromet., 5, 487-503.
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Data Set Citation
Dataset Originator/Creator: Joyce, R. J., J. E. Janowiak, P. A. Arkin, and P. Xie
Dataset Title: CMORPH 0.25 degree 3-hourly precipitation estimates
Dataset Release Date: December 3, 2002
Dataset Release Place: NOAA CPC, Maryland
Dataset Publisher: NOAA CPC
Version: Version 1.0
Other Citation Details: Please See Metadata Summary FieldOnline Resource: http://www.cpc.noaa.gov/products/janowiak/cmorph_description.html
Start Date: 2002-12-03Stop Date: 2010-05-19
Latitude Resolution: 0.25 degree
Longitude Resolution: 0.25 degree
Horizontal Resolution Range: 10 km - < 50 km or approximately .09 degree - < .5 degree
Temporal Resolution: 3-hourly
Temporal Resolution Range: Hourly - < Daily
ISO Topic Category
Data Set Progress
Distribution Media: Online (FTP)
Distribution Size: 3.5 MB per day (compressed) or 45 MB (uncompressed)
Distribution Format: Binary
Phone: 301-763-8000 x 7544
Email: robert.joyce at noaa.gov
NOAA/NCEP/CPC 5200 Auth Road
City: Camp Springs
Province or State: MD
Postal Code: 20746
Email: johnj at essic.umd.edu
Cooperative Institute for Climate and Satellites University of Maryland
City: College Park
Province or State: MD
Postal Code: 20740-3823
Ferraro, R. R., 1997: SSM/I derived global rainfall estimates for climatological applications. J. Geophys. Res., 102, 16715-16735.
Ferraro, R. R., F. Weng, N. C. Grody and L. Zhao, 2000: Precipitation characteristics over land from the NOAA-15 AMSU sensor. Geophys. Res. Ltr., 27, 2669-2672.
Joyce, R. J., J. E. Janowiak, P. A. Arkin, and P. Xie, 2004: CMORPH: A method that ... produces global precipitation estimates from passive microwave and infrared data at high spatial and temporal resolution.. J. Hydromet., 5, 487-503.
Kummerow, C., Y. Hong, W. S. Olson, S. Yang, R. F. Adler, J. McCollum, R. Ferraro, G. Petty, D-B Shin, and T. T. Wilheit, 2001: Evolution of the Goddard profiling algorithm (GPROF) for rainfall estimatin from passive microwave sensors. J. Appl. Meteor., 40, 1801-1820.
Creation and Review Dates
DIF Creation Date: 2010-05-19
Last DIF Revision Date: 2010-08-17