A Stable Finite-Difference Scheme for Population Growth and Diffusion on a Map.
W P Petersen1,2, S Callegari1, G R Lake3
1Anthropological Institute and Museum, Univ. of Zürich, Zürich, Switzerland.
Plos One
|January 14, 2017
Summary
We developed a stable numerical method to simulate human population dispersal using the Fisher-Kolmogorov equation. This approach models population spread over maps, predicting human arrival times in the Americas.
Area of Science:
- Computational modeling
- Population dynamics
- Paleoecology
Background:
- The Fisher-Kolmogorov-Petrovski-Piskunov (FKPP) equation models population growth and diffusion.
- Simulating human dispersal requires stable numerical methods applicable to complex geographical and environmental changes.
Purpose of the Study:
- To present a stable, semi-implicit Godunov-type splitting method for FKPP equation simulations.
- To apply this method to model late Pleistocene human population dispersal across geographical maps.
Main Methods:
- Developed a general Godunov-type splitting procedure for numerical simulations.
- Implemented Neumann boundary conditions for simulations on a world map.
- Utilized Net Primary Productivity (NPP) as a proxy for carrying capacity.
Main Results:
- The semi-implicit procedure ensures high numerical stability.
- The model successfully simulates population dispersal over geographical landscapes.
- NPP data was used to predict human arrival times in the Americas during the late Pleistocene.
Conclusions:
- The developed numerical method is effective for simulating population dispersal.
- This approach provides insights into human migration patterns and timing.
- Paleovegetation and paleoclimate data, proxied by NPP, are crucial for accurate dispersal modeling.
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