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The natural regime of river runoff changes constantly as a result of the introduction of stream-regulating equipment, including dams and dikes.
In the pine savannas of New Mexico's high country, the natural regime was one of frequent, low-burning wildfires that crept through the underbrush for weeks or months at a time.
Land use, point sources and population density were the main factors, but additional elements were included by several regions, such as the change of the natural regime, artificial modifications of the shoreline, introduction of fish and fish-farming activities, mass recreation, and invasive species.
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Prolonged rains often cause floods, especially in areas where the natural regimes of the rivers have been disrupted by uncontrolled mining or agricultural activities.
However, they may also disrupt some ecological processes in the natural forests in their new environments, such as changing the natural regimes of gap formation (Geldenhuys 1996a), or changing the behavior of fruit/seed dispersers (Dean 1985).
We modeled hypothetical herbivory effects under three disturbance regimes: (1) a natural disturbance regime without fire suppression, (2) a natural disturbance regime with only fire suppression, and (3) an active fuels management regime in which forest management was used to reduce probabilities of severe wildfires and in which wildfires were suppressed.
Ecosystems and communities dependent on natural flow regime have already experienced the adverse impacts of altered flow regimes due to engineering interventions.
The experiments have been performed under natural convection regime.
The natural, untamed regime of the river was characterized by high spring floods (polovodye).
Poff, N. L. et al. The natural flow regime: a paradigm for river conservation and restoration.
This contrasts with the expectations regarding the natural fire regime of this region.
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