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Our results suggest that landscapes with slowly moving drainage divides might not reach equilibrium, and that river basin dynamics may contribute to setting the large-scale morphology of old cratonic landscapes.
Foreland extension is consistent with existing geodynamic models for the Apennines and could represent the effects of lithospheric bending: its recognition and documentation elsewhere could provide significant insights to improve our understanding of syn-orogenic basin dynamics.
We explain Holocene hydrological changes through analysis of changing zonal climatic influences linked to Congo Air Boundary (CAB) and Intertropical Convergence Zone (ITCZ) dynamics, the effects of which filter into the region via complex drainage basin dynamics.
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The methodology, successfully applied to the Niger basin, is proposed as a strategic tool for studying the watershed dynamics for any time and space scales.
We use results from a climate-forced rainfall-runoff model to explicitly simulate intra-basin hydrologic dynamics and understand localized sensitivity to climate warming.
Inherited structures such as lithosphere-scale weakness zones formed under paleo-stress fields play a significant role in basin and lithosphere dynamics under present-day stress fields (Cloetingh et al. 2010).
The resulting thermal and flow field may help to understand the relation between basin-scale fluid dynamics and temperature distribution.
further explains the significance of the plateau: 'Meteorological scientists warn that [environmental changes on the plateau] may have implications beyond Asia's river basins, as shifting dynamics of the atmospheric circulatory system over the plateau could change wind and monsoon patterns across much of the world.
Within a specific river basin, water and sediment dynamics, and the relationship between them, can be assessed to reflect the basin's functions and services.
The new methods improve simulations of the architecture of basin deposits through the dynamics within the slope stability and debris flow modules.
Therefore, supplying more water to the basin without considering the dynamics of the interrelated problems will eventually lead to increased water demand.
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