Olusola Samuel Ojo

Dr. Olusola Samuel Ojo


Research Focus & Metrics

Academic Career Length

8Years (2019-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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26 June 2022 in Scientific African
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Journal Article
Open access
OOOlusola Samuel Ojo
Olusola Samuel Ojo
SOSamuel Toluwalope Ogunjo
Samuel Toluwalope Ogunjo

10 November 2020 in Neural Computing and Applications
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OOOlusola Samuel Ojo
Olusola Samuel Ojo
BABabatunde Adeyemi
Babatunde Adeyemi
DODaniel Oluwagbenga Oluleye
Daniel Oluwagbenga Oluleye

29 October 2024 in Theoretical and Applied Climatology
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EOEmmanuel O. Ogolo
Emmanuel O. Ogolo
OOOlusola Samuel Ojo
Olusola Samuel Ojo
IOIsrael O. Olabisi
Israel O. Olabisi

1 September 2019 in Journal of Atmospheric and Solar-Terrestrial Physics
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Journal Article
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OOOlusola Samuel Ojo
Olusola Samuel Ojo
BAB. Adeyemi
B. Adeyemi
EOE.O. Ogolo
E.O. Ogolo

19 January 2021 in Earth Systems and Environment
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OOOlusola Samuel Ojo
Olusola Samuel Ojo
BABabatunde Adeyemi
Babatunde Adeyemi
EOEmmanuel Omonigho Ogolo
Emmanuel Omonigho Ogolo

6 September 2020 in Radio Science
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Journal Article
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IEI. Emmanuel
I. Emmanuel
OOOlusola Samuel Ojo
Olusola Samuel Ojo
OAOladipo Emmanuel Abe
Oladipo Emmanuel Abe
KAK. D. Adedayo
K. D. Adedayo
Anomalous propagation conditions may cause multipath fading and strong signal enhancement on terrestrial line of sight links or interference on transhorizon paths. In detecting this conditions, spatial distribution of vertical refractivity gradient and ducting index were estimated across Nigeria using atmospheric data obtained from Era5 archive of European Centre for Medium‐Range Weather Forecasts (ECMWF). Refractivity and refractivity gradient were calculated from the obtained temperature, relative humidity, and pressure data using International Telecommunication Union (ITU) recommendation expression. Vertical refractivity gradient (VRG) and ducting index (Di) were deducted from refractivity gradient and modified the refractivity gradient. Correlation between vertical refractivity gradient, Di, and latitude were also computed. The result shows that the VRG values range between −5 and −65 N units/km in the Coastal and Guinea Savannah regions, and between −30 and −95 N units/km in the Midland and Sahelian regions. The Di values range between 10 and 60 in the Coastal and Guinea Savannah regions, between −10 and 110 in Midland and Sahelian region. Likewise, superrefraction and ducting are more prominent in the northern part, while superrefraction with minor subrefraction were noticed in the south. The Di performed better than VRG in detecting propagation conditions. Correlation between VRG and latitude ranges between −0.75 and −0.92. Correlation between Di and latitude is between 0.84 and 0.95. The values of VRG decrease northward, while those of the Di increase northward. Both VRG and Di revealed high variability in the dry months than in the wet months.