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The latitudinal variability of oceanic rainfall properties and its implication for satellite retrievals: 2. The relationships between radar observables and drop size distribution parameters

Citation

Protat, A and Klepp, C and Louf, V and Petersen, WA and Alexander, SP and Barros, A and Leinonen, J and Mace, GG, The latitudinal variability of oceanic rainfall properties and its implication for satellite retrievals: 2. The relationships between radar observables and drop size distribution parameters, Journal of Geophysical Research: Atmospheres, 124, (23) pp. 13312-13324. ISSN 2169-8996 (2019) [Refereed Article]


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Copyright Statement

Copyright 2019 Australian Bureau of Meteorology, Commonwealth of Australia

DOI: doi:10.1029/2019JD031011

Abstract

In this study, we develop statistical relationships between radar observables and drop size distribution properties in different latitude bands to inform radar rainfall retrieval techniques and understand underpinning microphysical reasons for differences reported in the literature between satellite mean zonal rainfall products at high latitudes (up to a factor 2 between products over ocean). A major assumption in satellite retrievals is the attenuation‐reflectivity relationships for convective and stratiform precipitation. They are found to systematically produce higher attenuation than our relationships with all latitudes included or within individual latitude bands (except in the tropics). The scatter around fitted curves approximating the radar reflectivity‐mass‐weighted diameter Dm relationship and the dual‐frequency ratio (ratio of Ka‐ to Ku‐band reflectivities)‐Dm relationships is found to be large and of the same magnitude. This result suggests that the added value of two radar frequencies to improve the Dm retrieval from space seems limited. In contrast, the relationship between Dm and the attenuation/reflectivity ratio is robust and not dependent on latitude. Direct relationships between rainfall and either reflectivity or attenuation are also found to be very robust. Attenuation‐reflectivity, Dm‐reflectivity, and rainfall rate‐reflectivity relationships in the Southern Hemisphere high latitude and Northern Hemisphere polar latitude bands are fundamentally different from those at other latitude bands, producing smaller attenuation, much larger Dm, and lower rainfall rates. This implies that specific relationships need to be used for these latitude bands in radar rainfall retrieval techniques using such relationships.

Item Details

Item Type:Refereed Article
Keywords:oceanic precipitation, satellite retrievals
Research Division:Earth Sciences
Research Group:Atmospheric sciences
Research Field:Cloud physics
Objective Division:Environmental Management
Objective Group:Air quality, atmosphere and weather
Objective Field:Atmospheric processes and dynamics
UTAS Author:Alexander, SP (Dr Simon Alexander)
ID Code:137573
Year Published:2019
Web of Science® Times Cited:3
Deposited By:Australian Antarctic Program Partnership
Deposited On:2020-02-20
Last Modified:2020-06-10
Downloads:6 View Download Statistics

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