GPM Ground Validation Dual Polarized C-Band Doppler Radar King City GCPExTable of Contents
The GPM Ground Validation Dual Polarized C-Band Doppler Radar King City GCPEx dataset includes special RHI and sector scans of several dual polarization parameters created by the C-Band radar during the GPM Cold-season Precipitation Experiment (GCPEx) in Ontario, Canada. Standard WKR IRIS volume and PPI scans, along with corresponding standard PPI imagery, are included. Additionally, specially configured CARE-centric composite images were also generated. Data was collected from January 15, 2012 through March 3, 2012. The following example shows how to cite the use of this dataset in a publication. For more information, please see our Citing GHRC DAAC and Data page. Campaign The GPM Cold-season Precipitation Experiment (GCPEx) occurred in Ontario, Canada during the winter season of 2011-2012. GCPEx addressed shortcomings in the GPM snowfall retrieval algorithm by collecting microphysical properties, associated remote sensing observations, and coordinated model simulations of precipitating snow. These data sets were collected to aid in the achievement of the over arching goal of GCPEx which is to characterize the ability of multi-frequency active and passive microwave sensors to detect and estimate falling snow. Further details on GCPEx are available at http://gpm.nsstc.nasa.gov/gcpex. Information on the Global Precipitation Measurement (GPM) mission is available at http://pmm.nasa.gov/GPM. The Environment Canada C-band dual polarization Doppler radar is located in King City, Canada. The location of the King City radar is:
The radar has the following characteristics:
More information on the WKR radar task configurations can be found in the GCPEx Task Configuration document. David Hudak The GPM Ground Validation Dual Polarized C-Band Doppler Radar King City GCPEx data files are named with the following convention:
where,
The GPM Ground Validation Dual Polarized C-Band Doppler Radar King City GCPEx dataset consists of binary files in the .iri format. The .iri format is a file extension of Vaisala's Interactive Radar Information System (IRIS). More information on IRIS can be found at Vaisala's IRIS web page. Browse files are also available in .gif format. The browse files also include specially configured CARE-centric composite images of both Z and ZDR products. RHI Scans The RHI scan files (gcpex_YYYYMMDD_HHMMSS_rhi_care.iri and gcpex_YYYYMMDD_HHMMSS_rhi_sat.iri) were created for each GCPEx ground site and include the following parameters: T, Z, ZDR, RHOV, PHIDP, KDP, SQI, WID, and VEL. The azimuth angle for each site is listed in the table below:
Browse images for the Z, ZDR, RHOHV, and PHIDP parameters of the RHI scan files were also created. Sector Scans The sector scans (gcpex_wkr_YYYYMMDD_HHMMSS_sector.iri) include the following parameters: T, Z, ZDR, RHOV, PHIDP, KDP, SQI, WID, and VEL at azimuth angles ranging from 290 - 359°. The angle numbers and elevation angles are listed in the table below:
Z products were created for the 12 elevations and ZDR, RHOHV, and PHIDP for the lowest angle only. At times on February 29, 2012, only the lowest 2 angles were scanned. Browse images are available for Z, ZDR, RHOHV, and PHIDP for certain elevation angles. CONVOL Volume Scans The CONVOL volume scans (gcpex_wkr_YYYYMMDDHHMM_convol_.iri) include the following parameters: T, Z, ZDR, RHOV, PHIDP, KDP, SQI, WID, and VEL. The angle numbers and elevation angles are listed in the table below:
Browse images are available for the CONVOL volume scans at the chosen elevation angle of 0.2°. DOPVOL2 Long Range Doppler Scans The DOPVOL2 long range Doppler scans (gcpex_wkr_YYYYMMDDHHMM_dopvol2_.iri) include the following variables: Z, T, VEL, and WID and were scanned at a PPI angle of 0.0°. Browse images are also available for these scans. POLPPI High Resolution PPI Scans The POLPPI high resolution PPI scans (gcpex_wkr_YYYYMMDDHHMM_polppi_.iri) include the following parameters: T, Z, ZDR, RHOV, PHIDP, KDP, SQI, WID, and VEL at a single PPI scan angle of 0.3°. Browse images are also available for these scans. Boodoo, S., D. Hudak, N. Donaldson, and M. Leduc. 2010. "Application of Dual-Polarization Radar Melting-Layer Detection Algorithm." Journal Of Applied Meteorology & Climatology 49, no. 8: 1779-1793. Hudak, D., P. Rodriguez, G. Lee, A. Ryzhkov, F. Fabry, and N. Donaldson. 2006. "Winter Precipitation Studies with a Dual Polarized C-band Radar."4th European Conference on Radar in Meteorology and Hydrology. Barcelona, Spain, 18-22 Sep, 2006. Contact InformationTo order these data or for further information, please contact:
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