Julia Atayi

Mx. Julia Atayi

Civil and Environmental Engineering, Morgan State University, Baltimore, Maryland, USA
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Research Focus & Metrics

Academic Career Length

4Years (2023-Present)

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

Representative Publications

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26 September 2023 in Theoretical and Applied Climatology
Verified
Journal Article
Closed access
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JAJulia Atayi
Julia Atayi
GAGeophrey K. Anornu
Geophrey K. Anornu
Alfred AwotwiAlfred Awotwi
Alfred Awotwi
SASamuel A. Andam-Akorful
Samuel A. Andam-Akorful
AKAmos T. Kabo-Bah
Amos T. Kabo-Bah
MAMaxwell Anim-Gyampo
Maxwell Anim-Gyampo

26 February 2025 in Hydrology
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Journal Article
Open access
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JAJulia Atayi
Julia Atayi
XZXin Zhou
Xin Zhou
Christos IliadisChristos Iliadis
Christos Iliadis
Vassilis GlenisVassilis Glenis
Vassilis Glenis
dong hee kangdong hee kang
dong hee kang
JHJames Gregory Hunter
James Gregory Hunter
Pluvial flooding, driven by increasingly impervious surfaces and intense storm events, presents a growing challenge for urban areas worldwide. In Baltimore City, MD, USA, climate change, rapid urbanization, and aging stormwater infrastructure are exacerbating flooding impacts, resulting in significant socio-economic consequences. This study evaluated the effectiveness of a soil profile rehabilitation scenario using a 2D hydrodynamic modeling approach for the Tiffany Run watershed, Baltimore City. This study utilized different extreme storm events, a high-resolution (1 m) LiDAR Digital Terrain Model (DTM), building footprints, and hydrological soil data. These datasets were integrated into a fully coupled 2D hydrodynamic model, the City Catchment Analysis Tool (CityCAT), to simulate urban flood dynamics. The pre-soil rehabilitation simulation revealed a maximum water depth of 3.00 m in most areas, with hydrologic soil groups C and D, especially downstream of the study area. The post-soil rehabilitation simulation was targeted at vacant lots and public parcels, accounting for 33.20% of the total area of the watershed. This resulted in a reduced water depth of 2.50 m. Additionally, the baseline runoff coefficient of 0.49 decreased to 0.47 following the rehabilitation, and the model consistently recorded a peak runoff reduction rate of 4.10 across varying rainfall intensities. The validation using a contingency matrix demonstrated true-positive rates of 0.75, 0.50, 0.64, and 0 for the selected events, confirming the model’s capability at capturing real-world flood occurrences.