Comparison of cloud-top topography and rainfall rates at the surface revealed that the areas of heavy rain are located where there are depressions at the anvil top. It was also found that the Z-R relationships show a large scatter when vertical and/or horizontal air currents are strong. Results of this research led to Project NIMROD proposed to begin in May 1978.
Mesoanalysis of record Chicago rainstorm using radar, satellite, and rain-gage data
1977-01-01
Conference paper
No indication
English
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