Premium
On the variability of the shape‐slope parameter relations of the gamma raindrop size distribution model
Author(s) -
Narayana Rao T.,
Kirankumar N. V. P.,
Radhakrishna B.,
Narayana Rao D.
Publication year - 2006
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2006gl028440
Subject(s) - disdrometer , environmental science , atmospheric sciences , variation (astronomy) , radar , meteorology , climatology , geology , precipitation , physics , rain gauge , astrophysics , computer science , telecommunications
The gamma parameters have been derived on the ground with the disdrometer and aloft with VHF and UHF radar measurements made at Gadanki in the southwest monsoon season. They have been used to study the variability of the shape‐slope ( μ ‐ Λ) relation with the climatic regime and also as a function of height. The μ ‐ Λ relation obtained at Gadanki differs from that derived at Florida and Oklahoma indicating climatic differences in the relation, which could be due to the microphysical differences in the rain DSD at these two locations. However, these differences could also arise due to the use of different type of disdrometers at these locations. For the first time, an attempt has been made to study the variation of this relation with height, and the analysis clearly reveals a significant variation in the coefficients of the relation with height. The vertical variability of the relation has been ascribed to the microphysical processes occurring in the height region concerned in the present study. These results suggest that for accurate retrieval of drop size distribution from polarimetric measurements and also for studies on the microphysics of rain systems, the vertical variability of the relation needs to be accounted, in particular in an environment where the DSD variations are considerable. In addition, the reduction of the scatter in the μ ‐ Λ plot after filtering light rain events, suggests that the μ ‐ Λ relation may be pertinent to moderate to heavy rain corroborating some of the earlier reports.