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Updated: May 5, 2026

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A Protocol for Conducting Rainfall Simulation to Study Soil Runoff
Published on: April 3, 2014
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A global parametric rain model for landfalling tropical cyclones: a case study for the U.S
King Heng Lau1, Sacha Czernichow1,2, Nathan Sparks1
1Department of Physics, Imperial College London, London, SW7 2AZ UK.
Summary
Tropical cyclone (TC) rainfall poses significant hazards, but estimating risk is difficult. A new model integrated with the Imperial College Storm Model (IRIS) simulates TC rain risk and projects increased rainfall under global warming.
Area of Science:
- Atmospheric Science
- Climate Science
- Meteorology
Background:
- Tropical cyclone (TC) rainfall is a major hazard, but its risk is hard to estimate due to infrequent events.
- Parametric TC rain models and stochastic risk models are essential for quantifying TC rain risk.
Purpose of the Study:
- Introduce a novel parametric rain model for landfalling TCs within the Imperial College Storm Model (IRIS).
- Quantify global TC rain risk and assess climate change impacts on hurricane rainfall in the United States.
Main Methods:
- Developed a new parametric rain model for landfalling TCs, integrated into the IRIS statistical-thermodynamic global TC hazard model.
- Conducted a 10,000-year simulation to reproduce observed global TC rain risk metrics.
- Applied a storyline approach to a +2°C global warming scenario for US hurricane rainfall projections.
Main Results:
- The IRIS model accurately reproduces global TC landfall rain rate, volume, and lifetime production return periods.
- For US hurricanes under +2°C warming, rain rates increase by 20.1%, storm-total volume by 3.9%, and lifetime rainfall by 14.6%.
- Warming enhances rainfall across the eastern and southern US, with greater inland and poleward penetration.
Conclusions:
- The new IRIS model effectively quantifies TC rain risk and provides valuable climate projection capabilities.
- Global warming intensifies hurricane rainfall, particularly in specific regions, leading to increased inland and poleward rainfall extent.
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