Think globally; act locally: I build large-scale models that preserve local flood characteristics.
Marcus N. Gomes Jr., PhD Hydrologist
I am interested in floods and extreme events, especially how their physical drivers and impacts change across scales. My work began with urban floods and open-source numerical models in Brazil. It now connects high-resolution hydrologic and hydrodynamic simulation, Earth observation, field measurements, data assimilation, and machine learning across Brazil, India, California, and the continental United States.
02 · Academic path
From engineering and hydraulics in Brazil to water resources engineering and hydrology in the US.
2013–2017
State University of Maringá
B.Sc., Civil Engineering
Teaching and undergraduate research on urban flood mitigation.
2018–2023
University of São Paulo
M.Sc. and Ph.D., Hydrology & Water Resources
Open-source flood modeling, design rainfall, and nature-based drainage. Best 2023 engineering thesis at EESC-USP.
2020–Present
University of Texas at San Antonio
Ph.D. studies, Civil & Environmental Engineering
Urban drainage, permeable pavement, field monitoring, and real-time control.
2024–2026
University of Arizona
Postdoctoral Research Associate
Hillslope hydrology and data assimilation at the Landscape Evolution Observatory.
2026–Present
Stanford University
Postdoctoral Researcher
Flood reconstruction across scales and the human consequences of exposure.
03 · Research program
How can large-scale flood models remain useful for local decisions?
Flood impacts are local, but national and global models cannot represent every street, channel, and drainage system. Coarser models smooth the terrain, hydraulic connectivity, storage, and infrastructure that control where water accumulates. Running meter-scale physically-based models across countries remains computationally prohibitive, and we still do not know which local characteristics coarse models must preserve. I work on this gap so large-scale regional or global models can support local decisions.
Where, when, and how deeply did floodwater accumulate?
Build multi-decade flood reconstructions by assimilating satellites, gauges, cameras, low-cost sensors, and community observations into physical models.
How should flood physics be represented as scale changes?
Simplify rainfall, terrain, storage, infrastructure, and surface–subsurface exchange systematically, then measure what changes inside the flooded domain, not only at the outlet.
Reference
Fine-grid process simulations
Target
Meter-scale to kilometer-scale resolution
Question 03 / Adaptation
How do scaling errors change adaptation and prediction?
Compare distributed nature-based solutions with conventional infrastructure under changing rainfall, land use, and aging systems, including cost and transferred risk.
Evaluation
Hazard · vulnerability · exposure
Decision test
Performance · feasibility · equity
04 · Selected publications
Recent papers on the research topic
Peer-reviewed first-author publications spanning hillslope-scale processes, catchment-scale processes, and multi-hazard continental vulnerability and exposure.
Water Resources Research
Research article · 2026
Identifying the State Dependence of Effective Material Properties
Simplified hillslope models can achieve greater accuracy by incorporating observations of groundwater depth and seepage (KGE from 0.85 to 0.96).
Spatio-temporal Performance of 2D Local-inertial Models
A formulation preserved maximum flood extent twenty times faster, while arrival time and velocity still changed. These variables determine local warning and hazard.