<Tr> <Td> 140 </Td> <Td> 224 </Td> <Td> 4.25 </Td> <Td> 108 </Td> </Tr> <Tr> <Td> 280 </Td> <Td> 448 </Td> <Td> 1.18 </Td> <Td> 30 </Td> </Tr> <P> Isaac Cline was the first to investigate rainfall distribution around tropical cyclones in the early 1900s . He found that a larger proportion of rainfall falls in advance of the center (or eye) than after the center's passage, with the highest percentage falling in the right front quadrant . Father Viñes of Cuba found that some tropical cyclones have their highest rainfall rates in the rear quadrant within a training (non-moving) inflow band . Normally, as a tropical cyclone intensifies, its heavier rainfall rates become more concentrated around its center . Rainfall is found to be heaviest in tropical cyclone's inner core, whether it be the eyewall or central dense overcast, within a degree latitude of the center, with lesser amounts farther away from the center . Most of the rainfall in tropical cyclones is concentrated within its radius of gale - force (34 knots / 39 mph / 63 km / h) winds . Rainfall is more common near the center of tropical cyclones overnight . Over land, outer bands are more active during the heating of the day, which can act to restrict inflow into the center of the cyclone . Recent studies have shown that half of the rainfall within a tropical cyclone is stratiform in nature . The chart to the right was developed by Riehl in 1954 using meteorological equations that assume a gale radius of about 140 miles (230 km), a fairly symmetric cyclone, and does not consider topographic effects or vertical wind shear . Local amounts can exceed this chart by a factor of two due to topography . Wind shear tends to lessen the amounts below what is shown on the table . </P> <P> Larger tropical cyclones have larger rain shields, which can lead to higher rainfall amounts farther from the cyclone's center . This is generally due to the longer time frame rainfall falls at any one spot in a larger system, when compared to a smaller system . Some of the difference seen concerning rainfall between larger and small storms could be the increased sampling of rainfall within a larger tropical cyclone when compared to that of a compact cyclone; in other words, the difference could be the result of a statistical problem . </P>

Where do you find precipitation in a cyclone
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