Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station

In this study, measurements of vertical profiles of rain parameters have been made using vertically pointing micro rain radar (VPMRR) at Akure (7.30° N, 5.13° E). Rain parameter data collected over seven-month rainfall episodes during the intense rainy season (April to October) have been analyzed fo...

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Main Authors: J.S. Ojo, D.B. Akoma, E.O. Olurotimi
Format: Article
Language:English
Published: Elsevier 2021-04-01
Series:Heliyon
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2405844021009919
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spelling doaj-45615845b4ff47d48c9b4e71dd8fb2192021-05-03T10:26:36ZengElsevierHeliyon2405-84402021-04-0174e06888Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical stationJ.S. Ojo0D.B. Akoma1E.O. Olurotimi2Department of Physics, The Federal University of Technology Akure, Nigeria; Corresponding author.Department of Physics, The Federal University of Technology Akure, NigeriaDepartment of Electronic Engineering, Durban University of Technology, KZN, 4000, South AfricaIn this study, measurements of vertical profiles of rain parameters have been made using vertically pointing micro rain radar (VPMRR) at Akure (7.30° N, 5.13° E). Rain parameter data collected over seven-month rainfall episodes during the intense rainy season (April to October) have been analyzed for a dynamical evolutionary trend over the site. Nearly all the episodes observed followed a similar pattern, hence, a single continuous rainfall episode occurring between 20:45:00 h and 21:14:00 h Greenwich Meridian Time (GMT) local time on 6th August 2018 is presented in this report. The results show no significant changes to the rain parameters (such as rain rate and liquid water content) nor contributed to the raindrop size distribution, based on average fall velocity of 6.55 m s−1 and rain rates within 1.3 and 2.6 mm h−1. This is to enable a stable fall for the dominant drops during the period. Further, the results revealed the transformation and collision of smaller drops to enhance a stable fall of larger drops during the rain event. The information from the study will be useful for radar meteorologists and microwave engineers in their designs.http://www.sciencedirect.com/science/article/pii/S2405844021009919Raindrop sizeRain typesVertical profileVPMRRTropical locationDynamical trend
collection DOAJ
language English
format Article
sources DOAJ
author J.S. Ojo
D.B. Akoma
E.O. Olurotimi
spellingShingle J.S. Ojo
D.B. Akoma
E.O. Olurotimi
Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station
Heliyon
Raindrop size
Rain types
Vertical profile
VPMRR
Tropical location
Dynamical trend
author_facet J.S. Ojo
D.B. Akoma
E.O. Olurotimi
author_sort J.S. Ojo
title Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station
title_short Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station
title_full Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station
title_fullStr Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station
title_full_unstemmed Dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station
title_sort dynamical evolution of vertical profile of rain structures observed using ground-based radar over a tropical station
publisher Elsevier
series Heliyon
issn 2405-8440
publishDate 2021-04-01
description In this study, measurements of vertical profiles of rain parameters have been made using vertically pointing micro rain radar (VPMRR) at Akure (7.30° N, 5.13° E). Rain parameter data collected over seven-month rainfall episodes during the intense rainy season (April to October) have been analyzed for a dynamical evolutionary trend over the site. Nearly all the episodes observed followed a similar pattern, hence, a single continuous rainfall episode occurring between 20:45:00 h and 21:14:00 h Greenwich Meridian Time (GMT) local time on 6th August 2018 is presented in this report. The results show no significant changes to the rain parameters (such as rain rate and liquid water content) nor contributed to the raindrop size distribution, based on average fall velocity of 6.55 m s−1 and rain rates within 1.3 and 2.6 mm h−1. This is to enable a stable fall for the dominant drops during the period. Further, the results revealed the transformation and collision of smaller drops to enhance a stable fall of larger drops during the rain event. The information from the study will be useful for radar meteorologists and microwave engineers in their designs.
topic Raindrop size
Rain types
Vertical profile
VPMRR
Tropical location
Dynamical trend
url http://www.sciencedirect.com/science/article/pii/S2405844021009919
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