Statistics of High Radar Reflectivity GradientsSource: Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 005::page 511Author:Mueller, E. A.
DOI: 10.1175/1520-0450(1977)016<0511:SOHRRG>2.0.CO;2Publisher: American Meteorological Society
Abstract: An analysis to determine the frequency of occurrence of gradients in reflectivity has been performed. Gradients as large as 50 dB km?1 occur with a frequency of over 1% of the pairs of adjacent nonzero reflectivities at ranges <32 km. At greater ranges, the observed gradients are less because of angular resolution of the radar. Considerable care must be taken in interpreting storm reflectivities if the logarithm of intensity or logarithm of power is averaged.
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contributor author | Mueller, E. A. | |
date accessioned | 2017-06-09T17:39:02Z | |
date available | 2017-06-09T17:39:02Z | |
date copyright | 1977/05/01 | |
date issued | 1977 | |
identifier issn | 0021-8952 | |
identifier other | ams-9266.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4232735 | |
description abstract | An analysis to determine the frequency of occurrence of gradients in reflectivity has been performed. Gradients as large as 50 dB km?1 occur with a frequency of over 1% of the pairs of adjacent nonzero reflectivities at ranges <32 km. At greater ranges, the observed gradients are less because of angular resolution of the radar. Considerable care must be taken in interpreting storm reflectivities if the logarithm of intensity or logarithm of power is averaged. | |
publisher | American Meteorological Society | |
title | Statistics of High Radar Reflectivity Gradients | |
type | Journal Paper | |
journal volume | 16 | |
journal issue | 5 | |
journal title | Journal of Applied Meteorology | |
identifier doi | 10.1175/1520-0450(1977)016<0511:SOHRRG>2.0.CO;2 | |
journal fristpage | 511 | |
journal lastpage | 513 | |
tree | Journal of Applied Meteorology:;1977:;volume( 016 ):;issue: 005 | |
contenttype | Fulltext |