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contributor authorChandrasekar, V.
contributor authorBringi, V. N.
date accessioned2017-06-09T15:22:36Z
date available2017-06-09T15:22:36Z
date copyright1988/12/01
date issued1988
identifier issn0739-0572
identifier otherams-420.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4180623
description abstractIn Part II of this study, simulations of multiparameter radar observables to include X-band specific attenuation (A) are performed in order to study the relationship between A, Z, and ZDR. We also compute the triplet (A, Z, ZDR) from simulations of disdrometer raindrop spectra. As in Part I, our simulations include the fluctuations due to both measurement errors and physical variations of the gamma raindrop spectra parameters (N0, D0, m). We examine the correlation between (A/Z) and ZDR derived from both disdrometer and radar simulations, and show that the disdrometer-based data yields a negative collation (? ?0.9) between (A/Z) and ZDR, whereas for radar data the correlation ≈ 0. We emphasize that these correlations are due only to measurement fluctuations, and not to physical variations. The large magnitude for the negative correlation compresses the scatter in plots of (A/Z) versus ZDR based on disdrometer RSD samples whereas the same scatter plots using multiparameter radar data show very large scatter. We also simulate A, Z and ZDR from three separate disdrometers (all sampling the same gamma RSD) and show that the scatter is more realistic and much larger than when using a single disdrometer.
publisherAmerican Meteorological Society
titleError Structure of Multiparameter Radar and Surface Measurements of Rainfall Part II: X-Band Attenuation
typeJournal Paper
journal volume5
journal issue6
journal titleJournal of Atmospheric and Oceanic Technology
identifier doi10.1175/1520-0426(1988)005<0796:ESOMRA>2.0.CO;2
journal fristpage796
journal lastpage802
treeJournal of Atmospheric and Oceanic Technology:;1988:;volume( 005 ):;issue: 006
contenttypeFulltext


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