University Of Tasmania
137573 - The latitudinal variability of oceanic rainfall properties and its implication.pdf (15.48 MB)
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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

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journal contribution
posted on 2023-05-20, 11:11 authored by Protat, A, Klepp, C, Louf, V, Petersen, WA, Simon AlexanderSimon Alexander, Barros, A, Leinonen, J, Mace, GG

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.


Publication title

Journal of Geophysical Research: Atmospheres










Institute for Marine and Antarctic Studies


Wiley-Blackwell Publishing Inc.

Place of publication

United States

Rights statement

Copyright 2019 Australian Bureau of Meteorology, Commonwealth of Australia

Repository Status

  • Open

Socio-economic Objectives

Atmospheric processes and dynamics